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  • 1
    Publication Date: 2020-12-23
    Description: Highlights • Sediment accumulation rates in Nicobar Fan abruptly increase 9.5 Ma. • Increased sediment flux to eastern Indian Ocean and restructuring of sediment routing. • Nicobar Fan holds significant record of Indian Ocean sedimentation in late Neogene. • Shillong Plateau and Indo–Burmese wedge uplift drive sediment south in late Miocene. A holistic view of the Bengal–Nicobar Fan system requires sampling the full sedimentary section of the Nicobar Fan, which was achieved for the first time by International Ocean Discovery Program (IODP) Expedition 362 west of North Sumatra. We identified a distinct rise in sediment accumulation rate (SAR) beginning ∼9.5 Ma and reaching 250–350 m/Myr in the 9.5–2 Ma interval, which equal or far exceed rates on the Bengal Fan at similar latitudes. This marked rise in SAR and a constant Himalayan-derived provenance necessitates a major restructuring of sediment routing in the Bengal–Nicobar submarine fan. This coincides with the inversion of the Eastern Himalayan Shillong Plateau and encroachment of the west-propagating Indo–Burmese wedge, which reduced continental accommodation space and increased sediment supply directly to the fan. Our results challenge a commonly held view that changes in sediment flux seen in the Bengal–Nicobar submarine fan were caused by discrete tectonic or climatic events acting on the Himalayan–Tibetan Plateau. Instead, an interplay of tectonic and climatic processes caused the fan system to develop by punctuated changes rather than gradual progradation.
    Type: Article , PeerReviewed
    Format: text
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  • 2
    Publication Date: 2020-02-06
    Description: Plate-boundary fault rupture during the 2004 Sumatra-Andaman subduction earthquake extended closer to the trench than expected, increasing earthquake and tsunami size. International Ocean Discovery Program Expedition 362 sampled incoming sediments offshore northern Sumatra, revealing recent release of fresh water within the deep sediments. Thermal modeling links this freshening to amorphous silica dehydration driven by rapid burial-induced temperature increases in the past 9 million years. Complete dehydration of silicates is expected before plate subduction, contrasting with prevailing models for subduction seismogenesis calling for fluid production during subduction. Shallow slip offshore Sumatra appears driven by diagenetic strengthening of deeply buried fault-forming sediments, contrasting with weakening proposed for the shallow Tohoku-Oki 2011 rupture, but our results are applicable to other thickly sedimented subduction zones including those with limited earthquake records.
    Type: Article , PeerReviewed
    Format: text
    Format: text
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  • 3
    Publication Date: 2023-02-08
    Description: Slow slip events (SSEs) accommodate a significant proportion of tectonic plate motion at subduction zones, yet little is known about the faults that actually host them. The shallow depth (〈2 km) of well-documented SSEs at the Hikurangi subduction zone offshore New Zealand offers a unique opportunity to link geophysical imaging of the subduction zone with direct access to incoming material that represents the megathrust fault rocks hosting slow slip. Two recent International Ocean Discovery Program Expeditions sampled this incoming material before it is entrained immediately down-dip along the shallow plate interface. Drilling results, tied to regional seismic reflection images, reveal heterogeneous lithologies with highly variable physical properties entering the SSE source region. These observations suggest that SSEs and associated slow earthquake phenomena are promoted by lithological, mechanical, and frictional heterogeneity within the fault zone, enhanced by geometric complexity associated with subduction of rough crust.
    Type: Article , PeerReviewed
    Format: text
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  • 4
    Publication Date: 2022-10-20
    Description: © The Author(s), 2021. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Vrolijk, P., Summa, L., Ayton, B., Nomikou, P., Huepers, A., Kinnaman, F., Sylva, S., Valentine, D., & Camilli, R. Using a Ladder of Seeps with computer decision processes to explore for and evaluate cold seeps on the Costa Rica active margin. Frontiers in Earth Science, 9, (2021): 601019, https://doi.org/10.3389/feart.2021.601019.
    Description: Natural seeps occur at the seafloor as loci of fluid flow where the flux of chemical compounds into the ocean supports unique biologic communities and provides access to proxy samples of deep subsurface processes. Cold seeps accomplish this with minimal heat flux. While individual expertize is applied to locate seeps, such knowledge is nowhere consolidated in the literature, nor are there explicit approaches for identifying specific seep types to address discrete scientific questions. Moreover, autonomous exploration for seeps lacks any clear framework for efficient seep identification and classification. To address these shortcomings, we developed a Ladder of Seeps applied within new decision-assistance algorithms (Spock) to assist in seep exploration on the Costa Rica margin during the R/V Falkor 181210 cruise in December, 2018. This Ladder of Seeps [derived from analogous astrobiology criteria proposed by Neveu et al. (2018)] was used to help guide human and computer decision processes for ROV mission planning. The Ladder of Seeps provides a methodical query structure to identify what information is required to confirm a seep either: 1) supports seafloor life under extreme conditions, 2) supports that community with active seepage (possible fluid sample), or 3) taps fluids that reflect deep, subsurface geologic processes, but the top rung may be modified to address other scientific questions. Moreover, this framework allows us to identify higher likelihood seep targets based on existing incomplete or easily acquired data, including MBES (Multi-beam echo sounder) water column data. The Ladder of Seeps framework is based on information about the instruments used to collect seep information (e.g., are seeps detectable by the instrument with little chance of false positives?) and contextual criteria about the environment in which the data are collected (e.g., temporal variability of seep flux). Finally, the assembled data are considered in light of a Last-Resort interpretation, which is only satisfied once all other plausible data interpretations are excluded by observation. When coupled with decision-making algorithms that incorporate expert opinion with data acquired during the Costa Rica experiment, the Ladder of Seeps proved useful for identifying seeps with deep-sourced fluids, as evidenced by results of geochemistry analyses performed following the expedition.
    Description: Support for this research was provided through NASA PSTAR Grant #NNX16AL08G and National Science Foundation Navigating the New Arctic grant #1839063. Use of the R/V Falkor and ROV SuBastian were provided through a grant from the Schmidt Ocean Institute. The AUG Nemesis and the Aurora in-situ mass spectrometer was provided through in-kind support from Teledyne Webb Research and Navistry Corp, respectively.
    Keywords: Seep ; Autonomous exploration ; Costa Rica ; Geochemistry ; Water column data ; Temporal variability ; Decision-making algorithm
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 5
    Publication Date: 2023-03-03
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 71 datasets
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  • 6
    Publication Date: 2023-03-03
    Keywords: Center for Marine Environmental Sciences; MARUM; Undrained shear strength
    Type: Dataset
    Format: application/zip, 139 datasets
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  • 7
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    PANGAEA
    In:  Supplement to: Ikari, Matt J; Hüpers, Andre; Kopf, Achim J (2013): Shear strength of sediments approaching subduction in the Nankai Trough, Japan as constraints on forearc mechanics. Geochemistry, Geophysics, Geosystems, 14(8), 2716-2730, https://doi.org/10.1002/ggge.20156
    Publication Date: 2023-05-12
    Description: The mechanical behavior of the plate boundary fault zone is of paramount importance in subduction zones, because it controls megathrust earthquake nucleation and propagation as well as the structural style of the forearc. In the Nankai area along the NanTroSEIZE (Kumano) drilling transect offshore SW Japan, a heterogeneous sedimentary sequence overlying the oceanic crust enters the subduction zone. In order to predict how variations in lithology, and thus mechanical properties, affect the formation and evolution of the plate boundary fault, we conducted laboratory tests measuring the shear strengths of sediments approaching the trench covering each major lithological sedimentary unit. We observe that shear strength increases nonlinearly with depth, such that the (apparent) coefficient of friction decreases. In combination with a critical taper analysis, the results imply that the plate boundary position is located on the main frontal thrust. Further landward, the plate boundary is expected to step down into progressively lower stratigraphic units, assisted by moderately elevated pore pressures. As seismogenic depths are approached, the décollement may further step down to lower volcaniclastic or pelagic strata but this requires specific overpressure conditions. High-taper angle and elevated strengths in the toe region may be local features restricted to the Kumano transect.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 8
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    PANGAEA
    Publication Date: 2023-03-03
    Keywords: Center for Marine Environmental Sciences; Elevation of event; Event label; GeoB23003-2; GeoB23004-2; GeoB23007-2; GeoB23008-2; GeoB23012-2; GeoB23016-1; GeoB23017-1; GeoB23018-1; GeoB23019-1; GeoB23021-1; GeoB23022-1; GeoB23023-1; GeoB23024-1; GeoB23025-1; GeoB23050-1; GeoB23050-2; GeoB23050-3; GeoB23050-4; GeoB23050-5; GeoB23050-6; GeoB23050-7; GeoB23070-1; GeoB23070-2; GeoB23074-1; GeoB23090-1; GeoB23090-2; GeoB23090-3; GeoB23090-4; GeoB23090-5; GeoB23090-6; GeoB23090-7; GeoB23090-8; GeoB23098-1; GeoB23098-2; GeoB23098-3; GeoB23098-4; heat flow; Heat flow; Heat-Flow probe; HF; Latitude of event; Lister-type marine heat flow probe; Location; Longitude of event; M149; M149_107-1; M149_107-2; M149_107-3; M149_107-4; M149_107-5; M149_107-6; M149_107-7; M149_107-8; M149_118-1; M149_118-2; M149_118-3; M149_118-4; M149_16; M149_17; M149_18; M149_19; M149_21; M149_22; M149_23; M149_24; M149_25; M149_27; M149_28; M149_29; M149_30; M149_31; M149_63-1; M149_63-2; M149_63-3; M149_63-4; M149_63-5; M149_63-6; M149_63-7; M149_85; M149_86-1; M149_89; MARUM; Meteor (1986); Optional event label
    Type: Dataset
    Format: text/tab-separated-values, 72 data points
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  • 9
    Publication Date: 2023-06-27
    Keywords: Center for Marine Environmental Sciences; DEPTH, sediment/rock; Fall Cone; GC; GeoB23049-1; Gravity corer; M149; M149_62; MARUM; Meteor (1986); Shear strength, undrained; Wykeham-Farrance cone penetrometer WF 21600
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 10
    Publication Date: 2023-06-27
    Keywords: Center for Marine Environmental Sciences; DEPTH, sediment/rock; Fall Cone; GC; GeoB23053-1; Gravity corer; M149; M149_67; MARUM; Meteor (1986); Shear strength, undrained; Wykeham-Farrance cone penetrometer WF 21600
    Type: Dataset
    Format: text/tab-separated-values, 8 data points
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