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  • 1
    Keywords: Sedimentary basins. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (127 pages)
    Edition: 1st ed.
    ISBN: 9789811305771
    Series Statement: Advances in Geological Science Series
    DDC: 552.5
    Language: English
    Note: Intro -- Preface -- Acknowledgements -- Contents -- 1 Tectonic Context of the Study Area -- 1.1 Plate Tectonic Framework of the Eastern Eurasian Margin -- 1.1.1 Chronicle of Plate Motions Since 100 Ma -- 1.1.2 Present-Day Configuration -- 1.2 Tectonic Epochs of Southwest Japan-Previous Studies -- 1.2.1 Paleomagnetism -- 1.2.2 Reflection Seismic Survey -- 1.3 Recent Crustal Movements Revealed by Geodetic Observation -- 1.4 Spatiotemporal Overview of the Osaka Sedimentary Basin -- 1.4.1 Paleogeography -- 1.4.2 Active Faults on Land -- 1.4.3 Geophysical Studies -- References -- 2 Basic Knowledge-Stratigraphy of the Osaka Group -- 2.1 Overview of Sedimentary Basins -- 2.2 Chronology -- 2.2.1 Biostratigraphy -- 2.2.2 Magnetostratigraphy -- 2.2.3 Tephrochronology -- 2.3 Paleoenvironment -- 2.4 Deep Boring Survey -- 2.4.1 Onshore Data -- 2.4.2 Offshore Data -- 2.5 Tectonic Movements Deduced from Burial History -- 2.5.1 Isotope Stage Boundaries -- 2.5.2 Subsurface Datum Levels -- 2.5.3 Differential Subsidence of Northern Osaka Basin -- References -- 3 Reflection Seismic Data -- 3.1 Dataset -- 3.2 Correlation Between Subsurface Datum Planes and Seismic Horizons -- 3.3 Systematic Descriptions -- 3.3.1 Data Acquired by Geological Survey of Japan, AIST -- 3.3.2 Data Acquired by Hydrographic and Oceanographic Department, JCG -- 3.3.3 Data Acquired by Hyogo Prefecture -- 3.3.4 Data Acquired by Osaka Soil Test Laboratory, GRI -- 3.3.5 Auxiliary Data -- 3.4 Results -- 3.4.1 Structural Architecture -- 3.4.2 Basin Accommodation -- References -- 4 Discussion-Origin and Evolution of the Osaka Basin -- 4.1 Comparison Between Proximal and Peripheral Parts of the Basin -- 4.2 Marine-Land Connectivity of Major Structural Trends -- 4.2.1 Awaji-Rokko Fault System and Osaka Bay Fault -- 4.2.2 N-S Warping Zones -- 4.2.3 Median Tectonic Line. , 4.2.4 Broad Contractional Horsts off the Eastern Coast of Awaji Island -- 4.3 Evolutionary Process of the Osaka Basin-A Tectonic Model -- 4.3.1 A Synthesis of the Plio-Pleistocene Tectonic Events -- 4.3.2 Structural Framework of the Present Osaka Basin -- References.
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  • 2
    Keywords: Earth sciences ; Earth Sciences ; Structural geology ; Sedimentology ; Geophysics ; Engineering geology ; Engineering Geology ; Foundations ; Hydraulics
    Description / Table of Contents: This publication shows the three-dimensional configuration of the gigantic tectonic sag of the Osaka Bay sedimentary basin on the eastern Eurasian margin based on reflection seismic data never before published. The basin has developed relatively quickly since the dawn of the Quaternary. High-resolution subsurface images on the profiles provide highly valuable information about the architecture of active faults, paleoenvironmental changes, and mass balance on the convergent margin. The book presents an excellent case study of a tectonically controlled basin because morphologies and evolutionary processes of such basins show an enormous diversity, reflecting spatiotemporal variation in tectonic stress. Furthermore, this volume provides insight into the general mechanism of sedimentary basin formation. The quantitative analyses contained here will be thought-provoking for industry experts, academics, and graduate and undergraduate students engaged in geologic survey and civil engineering. The contents will be especially useful to professionals in the fields of Quaternary geology, neotectonics, and active fault research
    Type of Medium: Online Resource
    Pages: Online-Ressource (X, 119 p. 80 illus., 59 illus. in color, online resource)
    ISBN: 9789811305771
    Series Statement: Advances in Geological Science
    Language: English
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  • 3
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    PANGAEA
    In:  Supplement to: Tarasov, Pavel E; Nakagawa, Takeshi; Demske, Dieter; Österle, Hermann; Igarashi, Yaeko; Kitagawa, Junko; Mokhova, Lyudmila M; Bazarova, Valentina B; Okuda, Masaaki; Gotanda, Katsuya; Miyoshi, Norio; Fujiki, Toshiyuki; Takemura, Keiji; Yonenobu, Hitoshi; Fleck, Andreas (2011): Progress in the reconstruction of Quaternary climate dynamics in the Northwest Pacific: A new modern analogue reference dataset and its application to the 430-kyr pollen record from Lake Biwa. Earth-Science Reviews, 108(1-2), 64-79, https://doi.org/10.1016/j.earscirev.2011.06.002
    Publication Date: 2023-05-12
    Description: This study presents a newly compiled dataset of modern pollen and climate data from 798 sites across Japan and the Russian Far East. This comprehensive reference dataset combined with the modern analogue technique (MAT) provides a powerful tool for pollen-based reconstruction of the Quaternary Northwest Pacific climate. Pollen-derived reconstruction of the modern climate at the reference pollen-sampling sites matches well with the estimated modern climate values (R2 values vary between 0.79 and 0.95, and RMSEP values vary between 5.8 and 9.7% of the modern climatic range for all nine tested variables). The successful testing of the method encourages its application to the fossil pollen records. We used a coarse-resolution pollen record from Lake Biwa to reconstruct glacial-interglacial climate dynamics in central Japan since ~438 kyr and compared it to the earlier reconstruction based on a less representative reference dataset. The current and earlier results consistently demonstrate that the coldest glacial intervals experienced pronounced cooling in winter and moderate cooling in summer, supporting the growth of cool mixed forest (COMX) where warm mixed forest (WAMX) predominates today. During the last glacial, maximum (~24 kyr BP) mean temperatures of the coldest (MTCO) and warmest (MTWA) month were about -13 °C (RMSEP = 2.34 °C) and 21 °C (RMSEP = 1.66 °C) respectively, and annual precipitation (PANN) was about 800 mm (RMSEP = 158.06 mm). During the thermal optimums of the interglacial intervals, the temperatures of the coldest and warmest month were above 0 °C and 25 °C respectively, leading to the reconstruction of WAMX and temperate conifer forest (TECO). Although both these vegetation types grow in the southern part of Japan today, WAMX requires warmer space. The presence of WAMX during marine isotope stages (MIS) 11 and 1, and its absence during MIS 9 and MIS 5 contradict the marine isotope and Antarctic ice records, suggesting that the latter two interglacials were the warmest of the last 800 kyr. The apparent contradiction allows at least three different explanations including low temporal resolution of the pollen record; different trends in CO2 concentrations during 'short' and 'long' interglacials; and regional climate variability and non-linear response of different regions to the global forcing. More definitive conclusions will be possible on the basis of forthcoming high-resolution pollen records from central Japan.
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 4
    Publication Date: 2023-05-12
    Keywords: AGE; DRILL; Drilling/drill rig; Japan; Lake_Biwa; Modern analog technique (MAT); Number of analogues; Precipitation, annual mean; Precipitation, annual mean, maximum; Precipitation, annual mean, minimum; Precipitation, Apr-Sep; Precipitation, Apr-Sep, maximum; Precipitation, Apr-Sep, minimum; Precipitation, Oct-Mar; Precipitation, Oct-Mar, maximum; Precipitation, Oct-Mar, minimum; Temperature, annual mean; Temperature, annual mean, maximum; Temperature, annual mean, minimum; Temperature, coldest month; Temperature, coldest month, maximum; Temperature, coldest month, minimum; Temperature, difference; Temperature, difference, maximum; Temperature, difference, minimum; Temperature, warmest month; Temperature, warmest month, maximum; Temperature, warmest month, minimum; Temperature coldness index; Temperature coldness index, maximum; Temperature coldness index, minimum; Temperature warmth index; Temperature warmth index, maximum; Temperature warmth index, minium
    Type: Dataset
    Format: text/tab-separated-values, 3780 data points
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  • 5
    Publication Date: 2023-05-12
    Keywords: AMUR1; AMUR10; AMUR11; AMUR12; AMUR13; AMUR14; AMUR15; AMUR16; AMUR17; AMUR18; AMUR19; AMUR2; AMUR20; AMUR21; AMUR22; AMUR23; AMUR24; AMUR25; AMUR26; AMUR27; AMUR28; AMUR29; AMUR3; AMUR31; AMUR32; AMUR33; AMUR34; AMUR35; AMUR36; AMUR37; AMUR38; AMUR39; AMUR4; AMUR40; AMUR43; AMUR44; AMUR45; AMUR46; AMUR47; AMUR48; AMUR49; AMUR5; AMUR50; AMUR51; AMUR52; AMUR53; AMUR54; AMUR55; AMUR56; AMUR57; AMUR6; AMUR7; AMUR8; AMUR9; China; DEPTH, sediment/rock; Elevation of event; Estimated by Polygon 2.3.3; Event label; Hand corer; HCOR; HOKK_02; HOKK_05; HOKK_07; HOKK_08; HOKK_10; HOKK_11; HOKK_14; Japan; Jss-001; Jss-002; Jss-003; Jss-004; Jss-005; Jss-006; Jss-007; Jss-008; Jss-009; Jss-010; Jss-011; Jss-012; Jss-013; Jss-014; Jss-015; Jss-016; Jss-017; Jss-018; Jss-019; Jss-020; Jss-021; Jss-022; Jss-023; Jss-024; Jss-025; Jss-026; Jss-027; Jss-028; Jss-029; Jss-030; Jss-031; Jss-032; Jss-033; Jss-034; Jss-035; Jss-036; Jss-037; Jss-038; Jss-039; Jss-040; Jss-041; Jss-042; Jss-043; Jss-044; Jss-045; Jss-046; Jss-047; Jss-048; Jss-049; Jss-050; Jss-051; Jss-052; Jss-053; Jss-054; Jss-055; Jss-056; Jss-057; Jss-058; Jss-059; Jss-060; Jss-061; Jss-062; Jss-063; Jss-064; Jss-065; Jss-066; Jss-067; Jss-068; Jss-069; Jss-070; Jss-071; Jss-072; Jss-073; Jss-074; Jss-075; Jss-076; Jss-077; Jss-078; Jss-079; Jss-080; Jss-081; Jss-082; Jss-083; Jss-084; Jss-085; Jss-086; Jss-087; Jss-088; Jss-089; Jss-090; Jss-091; Jss-092; Jss-093; Jss-094; Jss-095; Jss-096; Jss-097; Jss-098; Jss-099; Jss-100; Jss-101; Jss-102; Jss-103; Jss-104; Jss-105; Jss-106; Jss-107; Jss-108; Jss-109; Jss-110; Jss-111; Jss-112; Jss-113; Jss-114; Jss-115; Jss-116; Jss-117; Jss-118; Jss-119; Jss-120; Jss-121; Jss-122; Jss-123; Jss-124; Jss-125; Jss-126; Jss-127; Jss-128; Jss-129; Jss-130; Jss-131; Jss-132; Jss-133; Jss-134; Jss-135; Jss-136; Jss-137; Jss-138; Jss-139; Jss-140; Jss-141; Jss-142; Jss-143; Jss-144; Jss-145; Jss-146; Jss-147; Jss-148; Jss-149; Jss-150; Jss-151; Jss-152; Jss-153; Jss-154; Jss-155; Jss-156; Jss-157; Jss-158; Jss-159; Jss-160; Jss-161; Jss-162; Jss-163; Jss-164; Jss-165; Jss-166; Jss-167; Jss-168; Jss-169; Jss-170; Jss-171; Jss-172; Jss-173; Jss-174; Jss-175; Jss-176; Jss-177; Jss-178; Jss-179; Jss-180; Jss-181; Jss-182; Jss-183; Jss-184; Jss-185; Jss-186; Jss-187; Jss-188; Jss-189; Jss-190; Jss-191; Jss-192; Jss-193; Jss-194; Jss-195; Jss-196; Jss-197; Jss-198; Jss-199; Jss-200; Jss-201; Jss-202; Jss-203; Jss-204; Jss-205; Jss-206; Jss-207; Jss-208; Jss-209; Jss-210; Jss-211; Jss-212; Jss-213; Jss-214; Jss-215; Jss-216; Jss-217; Jss-218; Jss-219; Jss-220; Jss-221; Jss-222; Jss-223; Jss-224; Jss-225; Jss-226; Jss-227; Jss-228; Jss-229; Jss-230; Jss-231; Jss-232; Jss-233; Jss-234; Jss-235; Jss-236; Jss-237; Jss-238; Jss-239; Jss-240; Jss-241; Jss-242; Jss-243; Jss-244; Jss-245; Jss-246; Jss-247; Jss-248; Jss-249; Jss-250; Jss-251; Jss-252; Jss-253; Jss-254; Jss-255; Jss-256; Jss-257; Jss-258; Jss-259; Jss-260; Jss-261; Jss-262; Jss-263; Jss-264; Jss-265; Jss-266; Jss-267; Jss-268; Jss-269; Jss-270; Jss-271; Jss-272; Jss-273; Jss-274; Jss-275; Jss-276; Jss-277; Jss-278; Jss-279; Jss-280; Jss-281; Jss-282; Jss-283; Jss-284; Jss-285; Jun-286; Jun-287; Jun-288; Jun-289; Jun-290; Jun-291; Jun-292; Jun-293; Jun-294; Jun-295; Jun-296; Jun-297; Jun-298; Jun-299; Jun-300; Jun-301; Jun-302; Jun-303; Jun-304; Jun-305; Jun-306; Jun-307; Jun-308; Jun-310; Jun-311; Jun-312; Jun-313; Jun-314; Jun-315; Jun-316; Jun-317; Jun-318; Jun-319; Jun-320; Jun-321; Jun-322; Jun-323; Jun-324; Jun-325; Jun-326; Jun-327; Jun-328; KUNASH1; KUNASH2; KUNASH3; KUNASH4; KUNASH5; KUNASH6; KUNASH7; KUNASH8; Latitude of event; Longitude of event; MOKH1; MOKH10; MOKH100; MOKH101; MOKH102; MOKH103; MOKH104; MOKH105; MOKH106; MOKH107; MOKH108; MOKH109; MOKH11; MOKH110; MOKH111; MOKH112; MOKH113; MOKH114; MOKH115; MOKH116; MOKH117; MOKH118; MOKH119; MOKH12; MOKH120; MOKH121; MOKH122; MOKH123; MOKH124; MOKH125; MOKH126; MOKH127; MOKH128; MOKH129; MOKH13; MOKH130; MOKH131; MOKH133; MOKH134; MOKH135; MOKH136; MOKH137; MOKH138; MOKH139; MOKH14; MOKH140; MOKH141; MOKH142; MOKH143; MOKH144; MOKH145; MOKH146; MOKH147; MOKH148; MOKH149; MOKH15; MOKH150; MOKH151; MOKH152; MOKH153; MOKH154; MOKH155; MOKH156; MOKH157; MOKH158; MOKH159; MOKH16; MOKH160; MOKH161; MOKH162; MOKH163; MOKH164; MOKH165; MOKH166; MOKH167; MOKH168; MOKH169; MOKH17; MOKH170; MOKH171; MOKH172; MOKH173; MOKH174; MOKH175; MOKH176; MOKH177; MOKH178; MOKH18; MOKH180; MOKH181; MOKH182; MOKH183; MOKH184; MOKH185; MOKH186; MOKH187; MOKH188; MOKH189; MOKH19; MOKH194; MOKH195; MOKH196; MOKH197; MOKH199; MOKH2; MOKH200; MOKH202; MOKH204; MOKH206; MOKH207; MOKH208; MOKH209; MOKH21; MOKH210; MOKH211; MOKH212; MOKH213; MOKH214; MOKH215; MOKH216; MOKH217; MOKH218; MOKH219; MOKH22; MOKH220; MOKH221; MOKH223; MOKH224; MOKH225; MOKH226; MOKH227; MOKH228; MOKH23; MOKH231; MOKH233; MOKH234; MOKH237; MOKH238; MOKH239; MOKH24; MOKH240; MOKH241; MOKH242; MOKH25; MOKH26; MOKH27; MOKH28; MOKH29; MOKH3; MOKH30; MOKH31; MOKH32; MOKH33; MOKH34; MOKH35; MOKH36; MOKH38; MOKH39; MOKH40; MOKH41; MOKH42; MOKH43; MOKH44; MOKH45; MOKH46; MOKH47; MOKH48; MOKH49; MOKH50; MOKH51; MOKH53; MOKH54; MOKH55; MOKH56; MOKH59; MOKH6; MOKH60; MOKH61; MOKH62; MOKH63; MOKH64; MOKH65; MOKH66; MOKH67; MOKH68; MOKH69; MOKH7; MOKH71; MOKH72; MOKH73; MOKH75; MOKH76; MOKH77; MOKH78; MOKH79; MOKH8; MOKH80; MOKH81; MOKH82; MOKH83; MOKH84; MOKH85; MOKH86; MOKH87; MOKH88; MOKH89; MOKH9; MOKH91; MOKH92; MOKH93; MOKH94; MOKH95; MOKH96; MOKH97; MOKH98; MOKH99; Oku-013; Oku-014; Oku-015; Oku-016; Oku-017; Oku-018; Oku-019; Oku-020; Oku-021; Oku-022; Oku-023; Oku-024; Oku-025; Oku-026; Oku-027; Oku-028; Oku-029; Oku-030; Oku-031; Oku-035; Oku-036; Oku-037; Oku-038; Oku-039; Oku-040; Oku-041; Oku-042; Oku-043; Oku-044; Oku-045; Oku-046; Oku-047; Oku-048; Oku-051; Oku-052; Oku-053; Oku-054; Oku-055; Oku-056; Oku-057; Oku-058; Oku-059; Oku-060; Oku-061; Oku-062; Oku-063; Oku-064; Oku-065; Oku-066; Oku-067; Oku-068; Oku-069; Oku-070; Oku-071; Oku-072; Oku-073; Oku-074; Oku-075; Oku-076; Oku-077; Oku-078; Oku-079; Oku-080; Oku-081; Oku-082; Oku-083; Oku-084; Oku-085; Oku-086; Oku-087; Oku-088; Oku-089; Oku-090; Oku-091; Oku-092; Oku-093; Oku-094; Oku-095; Oku-096; Oku-097; Oku-098; Oku-099; Oku-100; Oku-101; Oku-102; Oku-103; Oku-105; Oku-106; Oku-107; Oku-108; Oku-109; Oku-110; Oku-111; Oku-112; Pav_1; Pav_10; Pav_11; Pav_12; Pav_13a; Pav_13b; Pav_14; Pav_15; Pav_16; Pav_17; Pav_18; Pav_19; Pav_2; Pav_20; Pav_21; Pav_22; Pav_23; Pav_24; Pav_25; Pav_3a; Pav_3b; Pav_3c; Pav_3d; Pav_4a; Pav_4b; Pav_4c; Pav_5; Pav_6; Pav_7; Pav_8; Pav_9; Pav_H12-1; Pav_H13-1; Pav_H13-2; Pav_H13-2(2); Pav_H13-3; Pav_H14-1; Pav_H14-2; Pav_H17-1; Pav_H17-2; Pav_H19-1; Pav_H19-2; Pav_H19-3; Pav_H19-4; Pav_H19-4bis; Pav_H19-5; Pav_H19-6; Pav_H20-1; Pav_H20-2; Pav_H20-3; Pav_H20-4; Pav_H20-5; Pav_H20-6; Precipitation, annual mean; Precipitation, Apr-Sep; Precipitation, Oct-Mar; Russia; SAKH_01; SAKH_03; SAKH_04; SAKH_06; SAKH_08; SAKH_10; SAKH_11; SAKH_13; SAKH_15; SAKH_17; SAKH_19; SAKH_21; SAKH_23; SAKH_25; SAKH_26; SAKH_28; SAKH_29; SAKH_31; SAKH_33; SAKH_35; SAKH_36; SAKH_37; SAKH_39; SAKH_40; SAKH_41; SAKH_43; SAKH_45; SAKH_47; SAKH_49; SAKH_51; SAKH_53; SAKH_54; SAKH_55; SAKH_57; SAKH_58; SAKH_59; SAKH_61; SAKH_62; SAKH_63; Temperature, annual mean; Temperature, coldest month; Temperature, difference; Temperature, warmest month; Temperature coldness index; Temperature gradient; Temperature warmth index
    Type: Dataset
    Format: text/tab-separated-values, 7980 data points
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  • 6
    Publication Date: 2023-05-12
    Keywords: AMUR1; AMUR10; AMUR11; AMUR12; AMUR13; AMUR14; AMUR15; AMUR16; AMUR17; AMUR18; AMUR19; AMUR2; AMUR20; AMUR21; AMUR22; AMUR23; AMUR24; AMUR25; AMUR26; AMUR27; AMUR28; AMUR29; AMUR3; AMUR31; AMUR32; AMUR33; AMUR34; AMUR35; AMUR36; AMUR37; AMUR38; AMUR39; AMUR4; AMUR40; AMUR43; AMUR44; AMUR45; AMUR46; AMUR47; AMUR48; AMUR49; AMUR5; AMUR50; AMUR51; AMUR52; AMUR53; AMUR54; AMUR55; AMUR56; AMUR57; AMUR6; AMUR7; AMUR8; AMUR9; China; DEPTH, sediment/rock; Event label; Hand corer; HCOR; HOKK_02; HOKK_05; HOKK_07; HOKK_08; HOKK_10; HOKK_11; HOKK_14; Japan; Jss-001; Jss-002; Jss-003; Jss-004; Jss-005; Jss-006; Jss-007; Jss-008; Jss-009; Jss-010; Jss-011; Jss-012; Jss-013; Jss-014; Jss-015; Jss-016; Jss-017; Jss-018; Jss-019; Jss-020; Jss-021; Jss-022; Jss-023; Jss-024; Jss-025; Jss-026; Jss-027; Jss-028; Jss-029; Jss-030; Jss-031; Jss-032; Jss-033; Jss-034; Jss-035; Jss-036; Jss-037; Jss-038; Jss-039; Jss-040; Jss-041; Jss-042; Jss-043; Jss-044; Jss-045; Jss-046; Jss-047; Jss-048; Jss-049; Jss-050; Jss-051; Jss-052; Jss-053; Jss-054; Jss-055; Jss-056; Jss-057; Jss-058; Jss-059; Jss-060; Jss-061; Jss-062; Jss-063; Jss-064; Jss-065; Jss-066; Jss-067; Jss-068; Jss-069; Jss-070; Jss-071; Jss-072; Jss-073; Jss-074; Jss-075; Jss-076; Jss-077; Jss-078; Jss-079; Jss-080; Jss-081; Jss-082; Jss-083; Jss-084; Jss-085; Jss-086; Jss-087; Jss-088; Jss-089; Jss-090; Jss-091; Jss-092; Jss-093; Jss-094; Jss-095; Jss-096; Jss-097; Jss-098; Jss-099; Jss-100; Jss-101; Jss-102; Jss-103; Jss-104; Jss-105; Jss-106; Jss-107; Jss-108; Jss-109; Jss-110; Jss-111; Jss-112; Jss-113; Jss-114; Jss-115; Jss-116; Jss-117; Jss-118; Jss-119; Jss-120; Jss-121; Jss-122; Jss-123; Jss-124; Jss-125; Jss-126; Jss-127; Jss-128; Jss-129; Jss-130; Jss-131; Jss-132; Jss-133; Jss-134; Jss-135; Jss-136; Jss-137; Jss-138; Jss-139; Jss-140; Jss-141; Jss-142; Jss-143; Jss-144; Jss-145; Jss-146; Jss-147; Jss-148; Jss-149; Jss-150; Jss-151; Jss-152; Jss-153; Jss-154; Jss-155; Jss-156; Jss-157; Jss-158; Jss-159; Jss-160; Jss-161; Jss-162; Jss-163; Jss-164; Jss-165; Jss-166; Jss-167; Jss-168; Jss-169; Jss-170; Jss-171; Jss-172; Jss-173; Jss-174; Jss-175; Jss-176; Jss-177; Jss-178; Jss-179; Jss-180; Jss-181; Jss-182; Jss-183; Jss-184; Jss-185; Jss-186; Jss-187; Jss-188; Jss-189; Jss-190; Jss-191; Jss-192; Jss-193; Jss-194; Jss-195; Jss-196; Jss-197; Jss-198; Jss-199; Jss-200; Jss-201; Jss-202; Jss-203; Jss-204; Jss-205; Jss-206; Jss-207; Jss-208; Jss-209; Jss-210; Jss-211; Jss-212; Jss-213; Jss-214; Jss-215; Jss-216; Jss-217; Jss-218; Jss-219; Jss-220; Jss-221; Jss-222; Jss-223; Jss-224; Jss-225; Jss-226; Jss-227; Jss-228; Jss-229; Jss-230; Jss-231; Jss-232; Jss-233; Jss-234; Jss-235; Jss-236; Jss-237; Jss-238; Jss-239; Jss-240; Jss-241; Jss-242; Jss-243; Jss-244; Jss-245; Jss-246; Jss-247; Jss-248; Jss-249; Jss-250; Jss-251; Jss-252; Jss-253; Jss-254; Jss-255; Jss-256; Jss-257; Jss-258; Jss-259; Jss-260; Jss-261; Jss-262; Jss-263; Jss-264; Jss-265; Jss-266; Jss-267; Jss-268; Jss-269; Jss-270; Jss-271; Jss-272; Jss-273; Jss-274; Jss-275; Jss-276; Jss-277; Jss-278; Jss-279; Jss-280; Jss-281; Jss-282; Jss-283; Jss-284; Jss-285; Jun-286; Jun-287; Jun-288; Jun-289; Jun-290; Jun-291; Jun-292; Jun-293; Jun-294; Jun-295; Jun-296; Jun-297; Jun-298; Jun-299; Jun-300; Jun-301; Jun-302; Jun-303; Jun-304; Jun-305; Jun-306; Jun-307; Jun-308; Jun-310; Jun-311; Jun-312; Jun-313; Jun-314; Jun-315; Jun-316; Jun-317; Jun-318; Jun-319; Jun-320; Jun-321; Jun-322; Jun-323; Jun-324; Jun-325; Jun-326; Jun-327; Jun-328; KUNASH1; KUNASH2; KUNASH3; KUNASH4; KUNASH5; KUNASH6; KUNASH7; KUNASH8; Modern analog technique (MAT); MOKH1; MOKH10; MOKH100; MOKH101; MOKH102; MOKH103; MOKH104; MOKH105; MOKH106; MOKH107; MOKH108; MOKH109; MOKH11; MOKH110; MOKH111; MOKH112; MOKH113; MOKH114; MOKH115; MOKH116; MOKH117; MOKH118; MOKH119; MOKH12; MOKH120; MOKH121; MOKH122; MOKH123; MOKH124; MOKH125; MOKH126; MOKH127; MOKH128; MOKH129; MOKH13; MOKH130; MOKH131; MOKH133; MOKH134; MOKH135; MOKH136; MOKH137; MOKH138; MOKH139; MOKH14; MOKH140; MOKH141; MOKH142; MOKH143; MOKH144; MOKH145; MOKH146; MOKH147; MOKH148; MOKH149; MOKH15; MOKH150; MOKH151; MOKH152; MOKH153; MOKH154; MOKH155; MOKH156; MOKH157; MOKH158; MOKH159; MOKH16; MOKH160; MOKH161; MOKH162; MOKH163; MOKH164; MOKH165; MOKH166; MOKH167; MOKH168; MOKH169; MOKH17; MOKH170; MOKH171; MOKH172; MOKH173; MOKH174; MOKH175; MOKH176; MOKH177; MOKH178; MOKH18; MOKH180; MOKH181; MOKH182; MOKH183; MOKH184; MOKH185; MOKH186; MOKH187; MOKH188; MOKH189; MOKH19; MOKH194; MOKH195; MOKH196; MOKH197; MOKH199; MOKH2; MOKH200; MOKH202; MOKH204; MOKH206; MOKH207; MOKH208; MOKH209; MOKH21; MOKH210; MOKH211; MOKH212; MOKH213; MOKH214; MOKH215; MOKH216; MOKH217; MOKH218; MOKH219; MOKH22; MOKH220; MOKH221; MOKH223; MOKH224; MOKH225; MOKH226; MOKH227; MOKH228; MOKH23; MOKH231; MOKH233; MOKH234; MOKH237; MOKH238; MOKH239; MOKH24; MOKH240; MOKH241; MOKH242; MOKH25; MOKH26; MOKH27; MOKH28; MOKH29; MOKH3; MOKH30; MOKH31; MOKH32; MOKH33; MOKH34; MOKH35; MOKH36; MOKH38; MOKH39; MOKH41; MOKH42; MOKH43; MOKH44; MOKH45; MOKH46; MOKH47; MOKH48; MOKH49; MOKH50; MOKH51; MOKH53; MOKH54; MOKH55; MOKH56; MOKH59; MOKH6; MOKH60; MOKH61; MOKH62; MOKH63; MOKH64; MOKH65; MOKH66; MOKH67; MOKH68; MOKH69; MOKH7; MOKH71; MOKH72; MOKH73; MOKH75; MOKH76; MOKH77; MOKH78; MOKH79; MOKH8; MOKH80; MOKH81; MOKH82; MOKH83; MOKH84; MOKH85; MOKH86; MOKH87; MOKH88; MOKH89; MOKH9; MOKH91; MOKH92; MOKH93; MOKH94; MOKH95; MOKH96; MOKH97; MOKH98; MOKH99; Number of analogues; Oku-013; Oku-014; Oku-015; Oku-016; Oku-017; Oku-018; Oku-019; Oku-020; Oku-021; Oku-022; Oku-023; Oku-024; Oku-025; Oku-026; Oku-027; Oku-028; Oku-029; Oku-030; Oku-031; Oku-035; Oku-036; Oku-037; Oku-038; Oku-039; Oku-040; Oku-041; Oku-042; Oku-043; Oku-044; Oku-045; Oku-046; Oku-047; Oku-048; Oku-051; Oku-052; Oku-053; Oku-054; Oku-055; Oku-056; Oku-057; Oku-058; Oku-059; Oku-060; Oku-061; Oku-062; Oku-063; Oku-064; Oku-065; Oku-066; Oku-067; Oku-068; Oku-069; Oku-070; Oku-071; Oku-072; Oku-073; Oku-074; Oku-075; Oku-076; Oku-077; Oku-078; Oku-079; Oku-080; Oku-081; Oku-082; Oku-083; Oku-084; Oku-085; Oku-086; Oku-087; Oku-088; Oku-089; Oku-090; Oku-091; Oku-092; Oku-093; Oku-094; Oku-095; Oku-096; Oku-097; Oku-098; Oku-099; Oku-100; Oku-101; Oku-102; Oku-103; Oku-105; Oku-106; Oku-107; Oku-108; Oku-109; Oku-110; Oku-111; Oku-112; Pav_1; Pav_10; Pav_11; Pav_12; Pav_13a; Pav_13b; Pav_14; Pav_15; Pav_16; Pav_17; Pav_18; Pav_19; Pav_2; Pav_20; Pav_21; Pav_22; Pav_23; Pav_24; Pav_25; Pav_3a; Pav_3b; Pav_3c; Pav_3d; Pav_4a; Pav_4b; Pav_4c; Pav_5; Pav_6; Pav_7; Pav_8; Pav_9; Pav_H12-1; Pav_H13-1; Pav_H13-2; Pav_H13-2(2); Pav_H13-3; Pav_H14-1; Pav_H14-2; Pav_H17-1; Pav_H17-2; Pav_H19-1; Pav_H19-2; Pav_H19-3; Pav_H19-4; Pav_H19-4bis; Pav_H19-5; Pav_H19-6; Pav_H20-1; Pav_H20-2; Pav_H20-3; Pav_H20-4; Pav_H20-5; Pav_H20-6; Precipitation, annual mean; Precipitation, annual mean, maximum; Precipitation, annual mean, minimum; Precipitation, Apr-Sep; Precipitation, Apr-Sep, maximum; Precipitation, Apr-Sep, minimum; Precipitation, Oct-Mar; Precipitation, Oct-Mar, maximum; Precipitation, Oct-Mar, minimum; Russia; SAKH_01; SAKH_03; SAKH_04; SAKH_06; SAKH_08; SAKH_10; SAKH_11; SAKH_13; SAKH_15; SAKH_17; SAKH_19; SAKH_21; SAKH_23; SAKH_25; SAKH_26; SAKH_28; SAKH_29; SAKH_31; SAKH_33; SAKH_35; SAKH_36; SAKH_37; SAKH_39; SAKH_40; SAKH_41; SAKH_43; SAKH_45; SAKH_47; SAKH_49; SAKH_51; SAKH_53; SAKH_54; SAKH_55; SAKH_57; SAKH_58; SAKH_59; SAKH_61; SAKH_62; SAKH_63; Temperature, annual mean; Temperature, annual mean, maximum; Temperature, annual mean, minimum; Temperature, coldest month; Temperature, coldest month, maximum; Temperature, coldest month, minimum; Temperature, difference; Temperature, difference, maximum; Temperature, difference, minimum; Temperature, warmest month; Temperature, warmest month, maximum; Temperature, warmest month, minimum; Temperature coldness index; Temperature coldness index, maximum; Temperature coldness index, minimum; Temperature warmth index; Temperature warmth index, maximum;
    Type: Dataset
    Format: text/tab-separated-values, 22316 data points
    Location Call Number Limitation Availability
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  • 7
    Publication Date: 2024-03-06
    Keywords: Abies; Acer; Aesculus; Alnus; AMUR1; AMUR10; AMUR11; AMUR12; AMUR13; AMUR14; AMUR15; AMUR16; AMUR17; AMUR18; AMUR19; AMUR2; AMUR20; AMUR21; AMUR22; AMUR23; AMUR24; AMUR25; AMUR26; AMUR27; AMUR28; AMUR29; AMUR3; AMUR31; AMUR32; AMUR33; AMUR34; AMUR35; AMUR36; AMUR37; AMUR38; AMUR39; AMUR4; AMUR40; AMUR43; AMUR44; AMUR45; AMUR46; AMUR47; AMUR48; AMUR49; AMUR5; AMUR50; AMUR51; AMUR52; AMUR53; AMUR54; AMUR55; AMUR56; AMUR57; AMUR6; AMUR7; AMUR8; AMUR9; Betula; Camellia; Carpinus; Castanopsis; China; Corylus; Counting, palynology; Cryptomeria; DEPTH, sediment/rock; Elevation of event; Ericaceae; Event label; Fagus; Fraxinus; Hand corer; HCOR; HOKK_02; HOKK_05; HOKK_07; HOKK_08; HOKK_10; HOKK_11; HOKK_14; Ilex; Japan; Jss-001; Jss-002; Jss-003; Jss-004; Jss-005; Jss-006; Jss-007; Jss-008; Jss-009; Jss-010; Jss-011; Jss-012; Jss-013; Jss-014; Jss-015; Jss-016; Jss-017; Jss-018; Jss-019; Jss-020; Jss-021; Jss-022; Jss-023; Jss-024; Jss-025; Jss-026; Jss-027; Jss-028; Jss-029; Jss-030; Jss-031; Jss-032; Jss-033; Jss-034; Jss-035; Jss-036; Jss-037; Jss-038; Jss-039; Jss-040; Jss-041; Jss-042; Jss-043; Jss-044; Jss-045; Jss-046; Jss-047; Jss-048; Jss-049; Jss-050; Jss-051; Jss-052; Jss-053; Jss-054; Jss-055; Jss-056; Jss-057; Jss-058; Jss-059; Jss-060; Jss-061; Jss-062; Jss-063; Jss-064; Jss-065; Jss-066; Jss-067; Jss-068; Jss-069; Jss-070; Jss-071; Jss-072; Jss-073; Jss-074; Jss-075; Jss-076; Jss-077; Jss-078; Jss-079; Jss-080; Jss-081; Jss-082; Jss-083; Jss-084; Jss-085; Jss-086; Jss-087; Jss-088; Jss-089; Jss-090; Jss-091; Jss-092; Jss-093; Jss-094; Jss-095; Jss-096; Jss-097; Jss-098; Jss-099; Jss-100; Jss-101; Jss-102; Jss-103; Jss-104; Jss-105; Jss-106; Jss-107; Jss-108; Jss-109; Jss-110; Jss-111; Jss-112; Jss-113; Jss-114; Jss-115; Jss-116; Jss-117; Jss-118; Jss-119; Jss-120; Jss-121; Jss-122; Jss-123; Jss-124; Jss-125; Jss-126; Jss-127; Jss-128; Jss-129; Jss-130; Jss-131; Jss-132; Jss-133; Jss-134; Jss-135; Jss-136; Jss-137; Jss-138; Jss-139; Jss-140; Jss-141; Jss-142; Jss-143; Jss-144; Jss-145; Jss-146; Jss-147; Jss-148; Jss-149; Jss-150; Jss-151; Jss-152; Jss-153; Jss-154; Jss-155; Jss-156; Jss-157; Jss-158; Jss-159; Jss-160; Jss-161; Jss-162; Jss-163; Jss-164; Jss-165; Jss-166; Jss-167; Jss-168; Jss-169; Jss-170; Jss-171; Jss-172; Jss-173; Jss-174; Jss-175; Jss-176; Jss-177; Jss-178; Jss-179; Jss-180; Jss-181; Jss-182; Jss-183; Jss-184; Jss-185; Jss-186; Jss-187; Jss-188; Jss-189; Jss-190; Jss-191; Jss-192; Jss-193; Jss-194; Jss-195; Jss-196; Jss-197; Jss-198; Jss-199; Jss-200; Jss-201; Jss-202; Jss-203; Jss-204; Jss-205; Jss-206; Jss-207; Jss-208; Jss-209; Jss-210; Jss-211; Jss-212; Jss-213; Jss-214; Jss-215; Jss-216; Jss-217; Jss-218; Jss-219; Jss-220; Jss-221; Jss-222; Jss-223; Jss-224; Jss-225; Jss-226; Jss-227; Jss-228; Jss-229; Jss-230; Jss-231; Jss-232; Jss-233; Jss-234; Jss-235; Jss-236; Jss-237; Jss-238; Jss-239; Jss-240; Jss-241; Jss-242; Jss-243; Jss-244; Jss-245; Jss-246; Jss-247; Jss-248; Jss-249; Jss-250; Jss-251; Jss-252; Jss-253; Jss-254; Jss-255; Jss-256; Jss-257; Jss-258; Jss-259; Jss-260; Jss-261; Jss-262; Jss-263; Jss-264; Jss-265; Jss-266; Jss-267; Jss-268; Jss-269; Jss-270; Jss-271; Jss-272; Jss-273; Jss-274; Jss-275; Jss-276; Jss-277; Jss-278; Jss-279; Jss-280; Jss-281; Jss-282; Jss-283; Jss-284; Jss-285; Juglans; Jun-286; Jun-287; Jun-288; Jun-289; Jun-290; Jun-291; Jun-292; Jun-293; Jun-294; Jun-295; Jun-296; Jun-297; Jun-298; Jun-299; Jun-300; Jun-301; Jun-302; Jun-303; Jun-304; Jun-305; Jun-306; Jun-307; Jun-308; Jun-310; Jun-311; Jun-312; Jun-313; Jun-314; Jun-315; Jun-316; Jun-317; Jun-318; Jun-319; Jun-320; Jun-321; Jun-322; Jun-323; Jun-324; Jun-325; Jun-326; Jun-327; Jun-328; KUNASH1; KUNASH2; KUNASH3; KUNASH4; KUNASH5; KUNASH6; KUNASH7; KUNASH8; Larix; Latitude of event; Longitude of event; MOKH1; MOKH10; MOKH100; MOKH101; MOKH102; MOKH103; MOKH104; MOKH105; MOKH106; MOKH107; MOKH108; MOKH109; MOKH11; MOKH110; MOKH111; MOKH112; MOKH113; MOKH114; MOKH115; MOKH116; MOKH117; MOKH118; MOKH119; MOKH12; MOKH120; MOKH121; MOKH122; MOKH123; MOKH124; MOKH125; MOKH126; MOKH127; MOKH128; MOKH129; MOKH13; MOKH130; MOKH131; MOKH133; MOKH134; MOKH135; MOKH136; MOKH137; MOKH138; MOKH139; MOKH14; MOKH140; MOKH141; MOKH142; MOKH143; MOKH144; MOKH145; MOKH146; MOKH147; MOKH148; MOKH149; MOKH15; MOKH150; MOKH151; MOKH152; MOKH153; MOKH154; MOKH155; MOKH156; MOKH157; MOKH158; MOKH159; MOKH16; MOKH160; MOKH161; MOKH162; MOKH163; MOKH164; MOKH165; MOKH166; MOKH167; MOKH168; MOKH169; MOKH17; MOKH170; MOKH171; MOKH172; MOKH173; MOKH174; MOKH175; MOKH176; MOKH177; MOKH178; MOKH18; MOKH180; MOKH181; MOKH182; MOKH183; MOKH184; MOKH185; MOKH186; MOKH187; MOKH188; MOKH189; MOKH19; MOKH194; MOKH195; MOKH196; MOKH197; MOKH199; MOKH2; MOKH200; MOKH202; MOKH204; MOKH206; MOKH207; MOKH208; MOKH209; MOKH21; MOKH210; MOKH211; MOKH212; MOKH213; MOKH214; MOKH215; MOKH216; MOKH217; MOKH218; MOKH219; MOKH22; MOKH220; MOKH221; MOKH223; MOKH224; MOKH225; MOKH226; MOKH227; MOKH228; MOKH23; MOKH231; MOKH233; MOKH234; MOKH237; MOKH238; MOKH239; MOKH24; MOKH240; MOKH241; MOKH242; MOKH25; MOKH26; MOKH27; MOKH28; MOKH29; MOKH3; MOKH30; MOKH31; MOKH32; MOKH33; MOKH34; MOKH35; MOKH36; MOKH38; MOKH39; MOKH40; MOKH41; MOKH42; MOKH43; MOKH44; MOKH45; MOKH46; MOKH47; MOKH48; MOKH49; MOKH50; MOKH51; MOKH53; MOKH54; MOKH55; MOKH56; MOKH59; MOKH6; MOKH60; MOKH61; MOKH62; MOKH63; MOKH64; MOKH65; MOKH66; MOKH67; MOKH68; MOKH69; MOKH7; MOKH71; MOKH72; MOKH73; MOKH75; MOKH76; MOKH77; MOKH78; MOKH79; MOKH8; MOKH80; MOKH81; MOKH82; MOKH83; MOKH84; MOKH85; MOKH86; MOKH87; MOKH88; MOKH89; MOKH9; MOKH91; MOKH92; MOKH93; MOKH94; MOKH95; MOKH96; MOKH97; MOKH98; MOKH99; Myrica; Oku-013; Oku-014; Oku-015; Oku-016; Oku-017; Oku-018; Oku-019; Oku-020; Oku-021; Oku-022; Oku-023; Oku-024; Oku-025; Oku-026; Oku-027; Oku-028; Oku-029; Oku-030; Oku-031; Oku-035; Oku-036; Oku-037; Oku-038; Oku-039; Oku-040; Oku-041; Oku-042; Oku-043; Oku-044; Oku-045; Oku-046; Oku-047; Oku-048; Oku-051; Oku-052; Oku-053; Oku-054; Oku-055; Oku-056; Oku-057; Oku-058; Oku-059; Oku-060; Oku-061; Oku-062; Oku-063; Oku-064; Oku-065; Oku-066; Oku-067; Oku-068; Oku-069; Oku-070; Oku-071; Oku-072; Oku-073; Oku-074; Oku-075; Oku-076; Oku-077; Oku-078; Oku-079; Oku-080; Oku-081; Oku-082; Oku-083; Oku-084; Oku-085; Oku-086; Oku-087; Oku-088; Oku-089; Oku-090; Oku-091; Oku-092; Oku-093; Oku-094; Oku-095; Oku-096; Oku-097; Oku-098; Oku-099; Oku-100; Oku-101; Oku-102; Oku-103; Oku-105; Oku-106; Oku-107; Oku-108; Oku-109; Oku-110; Oku-111; Oku-112; Pav_1; Pav_10; Pav_11; Pav_12; Pav_13a; Pav_13b; Pav_14; Pav_15; Pav_16; Pav_17; Pav_18; Pav_19; Pav_2; Pav_20; Pav_21; Pav_22; Pav_23; Pav_24; Pav_25; Pav_3a; Pav_3b; Pav_3c; Pav_3d; Pav_4a; Pav_4b; Pav_4c; Pav_5; Pav_6; Pav_7; Pav_8; Pav_9; Pav_H12-1; Pav_H13-1; Pav_H13-2; Pav_H13-2(2); Pav_H13-3; Pav_H14-1; Pav_H14-2; Pav_H17-1; Pav_H17-2; Pav_H19-1; Pav_H19-2; Pav_H19-3; Pav_H19-4; Pav_H19-4bis; Pav_H19-5; Pav_H19-6; Pav_H20-1; Pav_H20-2; Pav_H20-3; Pav_H20-4; Pav_H20-5; Pav_H20-6; Picea; Pinus; Podocarpus; Quercus, deciduous; Quercus evergreen; Reference/source; Rhododendron; Rhus; Russia; SAKH_01; SAKH_03; SAKH_04; SAKH_06; SAKH_08; SAKH_10; SAKH_11; SAKH_13; SAKH_15; SAKH_17; SAKH_19; SAKH_21; SAKH_23; SAKH_25; SAKH_26; SAKH_28; SAKH_29; SAKH_31; SAKH_33; SAKH_35; SAKH_36; SAKH_37; SAKH_39; SAKH_40; SAKH_41; SAKH_43; SAKH_45; SAKH_47; SAKH_49; SAKH_51; SAKH_53; SAKH_54; SAKH_55; SAKH_57; SAKH_58; SAKH_59; SAKH_61; SAKH_62; SAKH_63; Salix; Sciadopitys; Symplocos; Taxodiaceae; Tilia; Tsuga; Ulmus; Viburnum
    Type: Dataset
    Format: text/tab-separated-values, 26334 data points
    Location Call Number Limitation Availability
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  • 8
    Publication Date: 2024-04-20
    Keywords: Abrupt Climate Changes and Environmental Responses; Accumulation model; ACER; BIW95-4; Calendar age; Calendar age, maximum/old; Calendar age, minimum/young; Charcoal; Classical age-modeling approach, CLAM (Blaauw, 2010); DEPTH, sediment/rock; Lake Biwa; Sample ID; Type of age model; Unit
    Type: Dataset
    Format: text/tab-separated-values, 455 data points
    Location Call Number Limitation Availability
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  • 9
    Publication Date: 2024-04-20
    Keywords: Abies; Abrupt Climate Changes and Environmental Responses; Accumulation model; Acer; ACER; Aesculus; Alisma; Alnus; Amaranthaceae/Chenopodiaceae; Anemone; Apiaceae; Araliaceae; Artemisia; Asteraceae; Betula; BIW95-4; Brassicaceae; Buxus; Calendar age; Calendar age, maximum/old; Calendar age, minimum/young; Carpinus/Ostrya; Carpinus tschonoskii; Caryophyllaceae; Castanea/Castanopsis; Celastraceae; Celtis/Aphananthe; Cercidiphyllum; Classical age-modeling approach, CLAM (Blaauw, 2010); Cornus; Corylus; Counting, palynology; Cryptomeria; Cupressaceae-type; Cyperaceae; DEPTH, sediment/rock; Elaeagnaceae; Equisetum; Ericaceae; Eriocaulon; Fagus crenata; Fagus japonica; Fraxinus; Gentiana; Haloragis/Myriophyllum; Hemiptelea; Ilex; Impatiens; Isoetes; Juglans/Pterocarya; Lake Biwa; Lamiaceae; Larix; Ligustrum; Liliaceae; Lonicera; Lycopodium clavatum-type; Lycopodium inundatum-type; Lycopodium serratum-type; Lysichiton; Lythrum; Menyanthes; Myrica; Nuphar; Nymphoides; Nymphoides indica; Osmundaceae; Parthenocissus; Phellodendron; Picea; Pinus; Poaceae; Pollen indeterminata; Polygonum persicaria-type; Polygonum reynoutria-type; Polypodiales; Potamogeton; Pteridium; Pteridophyta; Quercus subgen. Cyclobalanopsis; Quercus subgen. Lepidobalanus; Ranunculus; Rhamnaceae; Rhus; Rosaceae; Rutaceae; Sagittaria; Salix; Sample ID; Sanguisorba; Sciadopitys; Sparganium/Trapa; Sparganium/Typha; Sphagnum; Styracaceae; Symplocos; Thalictrum; Tilia; Tsuga; Type of age model; Ulmus/Zelkova; Viburnum; Vitis
    Type: Dataset
    Format: text/tab-separated-values, 11013 data points
    Location Call Number Limitation Availability
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  • 10
    Electronic Resource
    Electronic Resource
    Melbourne, Australia : Blackwell Science Pty
    The @island arc 10 (2001), S. 0 
    ISSN: 1440-1738
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Abstract Drilling was carried out to penetrate the Nojima Fault where the surface rupture occurred associated with the 1995 Hyogo-ken Nanbu earthquake. Two 500 m boreholes were successfully drilled through the fault zone at a depth of 389.4 m. The drilling data show that the relative uplift of the south-east side of the Nojima Fault (south-west segment) was approximately 230 m. The Nojima branch fault, which branches from the Nojima Fault, is inferred to extend to the Asano Fault. From the structural contour map of basal unconformity of the Kobe Group, the vertical component of displacement of the Nojima branch–Asano Fault is estimated to be 260–310 m. Because the vertical component of displacement on the Nojima Fault of the north-east segment is a total of those of the Nojima Fault of the south-west segment and of the Nojima branch–Asano Fault, it is estimated to total to 490–540 m. From this, the average vertical component of the slip rate on the Nojima Fault is estimated to be 0.4–0.45 m/103 years for the past 1.2 million years.
    Type of Medium: Electronic Resource
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