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  • Li, Xiaohui  (11)
  • Wang, Xiaoyuan  (11)
  • 1
    In: Geology, Geological Society of America, Vol. 49, No. 10 ( 2021-10-01), p. 1165-1170
    Abstract: Molybdenum (Mo) isotope ratios provide a potential means of tracing material recycling involved in subduction zone processes. However, the geochemical behavior of Mo in subducted oceanic crust remains enigmatic. We analyzed Mo isotope ratios of arc and back-arc basin lavas from the Mariana subduction zone (western Pacific Ocean), combining newly obtained element and Sr-Nd-Pb-Li isotope data to investigate subduction zone geochemical processes involving Mo. The Mo isotope ratios (δ98/95MoNIST3134; U.S. National Institute of Standards and Technology [NIST] Mo standard) of the volcanic rocks showed clear across-arc variations, decreasing with increasing depth to the Wadati-Benioff zone. The high δ98/95Mo values in the Mariana Islands (−0.18‰ to +0.38‰) correspond to high 87Sr/86Sr, low 143Nd/144Nd, and radioge nic Pb isotope ratios, suggesting that altered upper oceanic crust played an important role in the magma source. The low δ98/95Mo values in the Central Mariana Trough (−0.65‰ to −0.17‰) with mantle-like Sr-Nd-Pb but slightly low δ7Li values provide direct evidence for the contribution of deep recycled oceanic crust to the magma source of the back-arc basin lavas. The isotopically light Mo magmas originated by partial melting of a residual subducted slab (eclogite) after high degrees of dehydration and then penetrated into the back-arc mantle. This interpretation provides a new perspective with which to investigate the deep recycling of subducted oceanic lithosphere and associated magma petrogenesis.
    Type of Medium: Online Resource
    ISSN: 0091-7613 , 1943-2682
    Language: English
    Publisher: Geological Society of America
    Publication Date: 2021
    detail.hit.zdb_id: 184929-3
    detail.hit.zdb_id: 2041152-2
    SSG: 13
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  • 2
    In: Geological Journal, Wiley, Vol. 53, No. 5 ( 2018-09), p. 1755-1766
    Abstract: Major element, trace element, and Sr–Nd–Pb isotopic compositions of high‐potassium calc‐alkaline rhyolites (the T6 rhyolites) collected from the western slope of the middle Okinawa Trough (MOT) are reported in this article. These high‐potassium rhyolites have similar major and trace elemental compositions as Type 2 rhyolites from the MOT, except that the former contain higher concentrations of K 2 O, Th, U, and Rb and lower concentrations of Sr and Eu. Experimental data indicate that the T6 rhyolites cannot be sourced from low‐ to mid‐potassium MOT rocks by either fractional crystallization or partial melting processes but are instead derived from a cryptic potassium‐rich source beneath the Okinawa Trough (OT). Considering that high‐potassium volcanic rocks are distributed throughout the East China Sea Shelf, the Ryukyu Arc, and Kyushu Island, the high‐potassium OT rocks could represent an important connection between the OT and its adjacent regions. Compared to volcanic rocks from the MOT axial zone, the T6 rhyolites have more depleted Sr–Nd isotopic compositions ( 87 Sr/ 86 Sr = 0.7035–0.7036, 143 Nd/ 144 Nd = 0.51291–0.51297) but much more enriched compositions of 207 Pb ( 207 Pb/ 204 Pb = 15.60–15.63) and 208 Pb ( 208 Pb/ 204 Pb = 38.45–38.57), thus recording a significant DUPAL‐like signature. These isotopic anomalies cannot be explained by the incorporation of subducting sediments or crustal contamination but instead imply the presence of a DUPAL‐like mantle source beneath the OT. The decrease of the DUPAL‐like anomaly from the T6 rhyolites to the MOT axial zone volcanic rocks is consistent with the injection of an normal mid‐ocean ridge basalt (N‐MORB) mantle source, such as asthenospheric material, into pre‐existing DUPAL‐like mantle during back‐arc extension.
    Type of Medium: Online Resource
    ISSN: 0072-1050 , 1099-1034
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2018
    detail.hit.zdb_id: 1479201-1
    SSG: 13
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  • 3
    In: Lithos, Elsevier BV, Vol. 360-361 ( 2020-05), p. 105444-
    Type of Medium: Online Resource
    ISSN: 0024-4937
    RVK:
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2020
    detail.hit.zdb_id: 1494884-9
    detail.hit.zdb_id: 221624-3
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  • 4
    In: Geological Journal, Wiley, Vol. 53, No. 6 ( 2018-11), p. 3129-3146
    Abstract: Silicate melt inclusions (SMIs) in basalt from the middle Okinawa Trough are investigated in detail to understand the source geochemical characteristics and petrogenesis of the basalt. The middle Okinawa Trough basalts contain abundant SMIs within olivine phenocrysts. The major element compositions of the SMIs are analysed using an electron microprobe. After correcting for olivine postentrapment crystallization, the major element compositions of the SMIs are more variable in terms of SiO 2 (49.7–54.8 wt%) and MgO (5.1–7.2 wt%) than those of the host basalt (SiO 2 , 52.4 wt%; MgO, 5.7 wt%), which could indicate the existence of more primitive melts than erupted bulk rock. The major element compositions of the SMIs indicate that the SMI‐recorded melt evolution process was mainly dominated by the fractional crystallization of olivine. According to laser ablation inductively coupled mass spectrometer analyses, the trace element compositions of the SMIs are similar to those of the host bulk rock and feature obvious enrichment in Pb and large‐ion lithophile elements relative to high field strength elements, rare earth elements, and highly negative Nb and Ta anomalies. The low Ce/Pb ratios, high Pb contents, and trace element distribution patterns in the SMIs are related to contributions from subducted sedimentary components in the magma source. Based on the electron microprobe analyses, the chemical composition of the olivine suggests that the lithology of the basalt source may be pyroxenite. The basalts may have been generated by the partial melting of pyroxenite during interactions between mantle‐wedge peridotite and Si‐rich melts that were released from the subducted slab.
    Type of Medium: Online Resource
    ISSN: 0072-1050 , 1099-1034
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2018
    detail.hit.zdb_id: 1479201-1
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  • 5
    In: Geological Journal, Wiley, Vol. 54, No. 3 ( 2019-05), p. 1160-1189
    Abstract: Silicate melt inclusions (SMIs) in olivine, clinopyroxene, and orthopyroxene in basalt and trachyandesite of the middle Okinawa Trough (MOT) and in basaltic andesites of the southern Okinawa Trough (SOT) were investigated in detail to understand the evolution of magma and geochemical characteristics of the basaltic magma source. Both the SMIs and host bulk rocks are more heavily enriched with Pb and large ion lithophile elements than with high field strength elements and rare earth elements. The major element compositions of SMIs in the MOT trachyandesite show a scattered variation trend of medium‐K to shoshonitic series and suggest that a K‐rich magma source may exist in the Okinawa Trough. Two groups with distinct element distribution patterns observed in SMIs of the MOT trachyandesite may represent magmas with different evolutionary histories. Compared with fractional crystallization and partial melting processes, magma mixing may serve as a reasonable process for the production of trachyandesite in the MOT. Fractional crystallization has played an important role in basaltic magma evolution in the MOT and SOT. Simulations conducted using MELTS show that the fractional crystallization evolution trends observed correspond well to the presence of a magma chamber at 300 MPa with an H 2 O content level of 0.2 wt% in the MOT and to the presence of a magma chamber at 300 MPa with an H 2 O content level of 0.4 wt% in the SOT. Ratios of incompatible trace elements (e.g., Th/Ce, Th/Sm, Ba/Th, and Th/Nb); positive Pb anomalies; negative Nb, Ta, and Ti anomalies; and the existence of organic hydrocarbons (C n H m ) in the SMIs can be attributed to the involvement of subducted sediment from the subducting slab. Modelling results suggest that more primitive magma represented by SMIs from the MOT has formed through the melting of less than 6% of a metasomatized depleted mantle with contributions of 1.2% sediment melt and 0.8% sediment fluid. In contrast, more primitive magma from the SOT formed through the melting of 4–10% of the depleted mantle with contributions of 3% sediment melt and 1% sediment fluid. The different features of the SMIs together with different tectonic settings of the MOT and SOT have formed in response to the westward subduction of the Philippine Sea Plate.
    Type of Medium: Online Resource
    ISSN: 0072-1050 , 1099-1034
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2019
    detail.hit.zdb_id: 1479201-1
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  • 6
    In: Lithos, Elsevier BV, Vol. 398-399 ( 2021-10), p. 106263-
    Type of Medium: Online Resource
    ISSN: 0024-4937
    RVK:
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2021
    detail.hit.zdb_id: 1494884-9
    detail.hit.zdb_id: 221624-3
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  • 7
    In: Geological Journal, Wiley, Vol. 54, No. 1 ( 2019-01), p. 316-332
    Abstract: In the southwestern Okinawa Trough, a cluster of approximate 70 submarine volcanoes is located at the cross back‐arc volcanic trail (CBVT), with the eruptive products dominated by rhyolites. New whole‐rock major and trace element and Sr–Nd–Pb–O isotopic data and previously available geochemistry data of volcanic rocks from this region are presented to determine the petrogenesis of these rhyolites. The rhyolites have high SiO 2 ( 〉 70.01 wt.%), K 2 O + Na 2 O (6.71–7.16 wt.%) contents and differentiation index (DI) values (DI  〉  93), and are metaluminous to weakly peraluminous (A/CNK = 0.99–1.11) and medium‐K calc‐alkaline in composition. The relatively low 10 4 *Ga/Al (2.06–2.17) and FeO*/MgO ratios (4.50–6.62), as well as Zr (91–174 ppm) and Zr + Ce + Nb + Y (175–271) contents suggest that the rhyolites, which contain hornblende, are generally similar to those of typical highly fractionated I‐type granitoids. The rhyolites show arc‐related features such as enrichment in LILEs (Rb, Ba, K), Th, U, Pb, and LREEs ((La/Yb) N  = 6.21–6.74) and strong depletion in HFSEs (Nb, Ta, P, Ti) with both nearly identical and more enriched isotopic compositions, including εNd (from −3.2 to −3.5), 87 Sr/ 86 Sr ratios (0.705552 to 0.705713), δ 18 O values (+8.1‰ to +8.6‰), and Pb isotopic compositions ( 206 Pb/ 204 Pb = 18.568–18.589, 207 Pb/ 204 Pb = 15.641–15.656, and 208 Pb/ 204 Pb = 38.848–38.904). Based on these characteristics, we propose that subduction‐related basalt magma and crust‐derived magma mixed and homogenized within a shallow magma chamber with a homogeneous “base‐level” isotopic signature of 〉 0·7055 ( 87 Sr/ 86 Sr) and 〉 −3 (εNd). This magma would have then experienced the extensive fractional crystallization of minerals, including plagioclase, hornblende, apatite, sphene, and Fe–Ti oxides, to form the CBVT rhyolites. Our geochemical interpretation of the existence of a long‐lived, convecting magma chamber beneath the CBVT is also consistent with seismic tomography results.
    Type of Medium: Online Resource
    ISSN: 0072-1050 , 1099-1034
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2019
    detail.hit.zdb_id: 1479201-1
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  • 8
    Online Resource
    Online Resource
    Springer Science and Business Media LLC ; 2017
    In:  Journal of Ocean University of China Vol. 16, No. 6 ( 2017-12), p. 1097-1108
    In: Journal of Ocean University of China, Springer Science and Business Media LLC, Vol. 16, No. 6 ( 2017-12), p. 1097-1108
    Type of Medium: Online Resource
    ISSN: 1672-5182 , 1993-5021
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2017
    detail.hit.zdb_id: 2274194-X
    SSG: 14
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  • 9
    In: Chemical Geology, Elsevier BV, Vol. 543 ( 2020-06), p. 119600-
    Type of Medium: Online Resource
    ISSN: 0009-2541
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2020
    detail.hit.zdb_id: 1492506-0
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  • 10
    In: Geofluids, Hindawi Limited, Vol. 2020 ( 2020-02-15), p. 1-18
    Abstract: The composition of hydrothermal plumes reflects the physical and chemical characteristics of seafloor hydrothermal fluids, which in turn reflects the host rock and subseafloor reaction conditions as well as the water column processes that act to alter the plumes as they disperse and age. Here, we show that the turbidity, current, pH value, dissolved Fe (dFe), and dissolved Mn (dMn) compositions of hydrothermal plumes can be used to understand the spatial distribution and source of hydrothermal systems in the submarine geological environment. Data were obtained from 18 hydrocast stations, among which the water column samples were collected at 8 stations during the MANUS cruise of R/V KEXUE in 2015. The results showed that the Satanic Mills plume and Fenway plume rose approximately 140 m and 220 m above the seafloor, respectively. In the Satanic Mills plume, dFe remained longer than dMn during lateral plume dispersal. There was a clear intersection of the Satanic Mills plume and Fenway plume between 1625 m and 1550 m in the PACMANUS hydrothermal field, and the varied dispersion trends of the mixed plumes were affected by current velocities at different depths. The physical and chemical properties of the seawater columns in the Manus Basin were affected by the input of high-Mn, high-Fe, and low-Mg vent fluids. The turbidity and dFe, dMn, and dissolved Mg concentrations in the sections of the plumes proximal to the Satanic Mills, Fenway, and Desmos vent sites were generally higher (turbidity, Mn, and Fe) and lower (Mg) than those in the sections of the plumes that were more distal from the vent sites. This implied that the plumes proximal to their vent fluid sources, which were interpreted to have relatively young ages, dispersed chemically over time, and their concentrations became more similar to those of the plumes that were more distal from their vent fluid sources.
    Type of Medium: Online Resource
    ISSN: 1468-8115 , 1468-8123
    Language: English
    Publisher: Hindawi Limited
    Publication Date: 2020
    detail.hit.zdb_id: 2045012-6
    SSG: 13
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