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Sedimentary and volcanic record of the nascent Izu-Bonin-Mariana arc from IODP Site U1438
Waldman, Ryan J.1,2; Marsaglia, Kathleen M.1; Hickey-Vargas, Rosemary3; Ishizuka, Osamu4,5; Johnson, Kyle E.1; McCarthy, Anders6,7; Yogodzinski, Gene2; Samajpati, Eshita3; Li, He8; Laxton, Kate9; Savov, Ivan P.9; Meffre, Sebastien10; Arculus, Richard J.11; Bandini, Alexandre N.12; Barth, Andrew P.13; Bogus, Kara14; Brandl, Philipp A.15; Gurnis, Michael16; Jiang, Fuqing17
2021-07-01
发表期刊GEOLOGICAL SOCIETY OF AMERICA BULLETIN
ISSN0016-7606
卷号133期号:7-8页码:1421-1440
通讯作者Marsaglia, Kathleen M.([email protected])
摘要The oldest known, intact sedimentary record of a nascent intraoceanic arc was recovered in a similar to 100-m-thick unit (IV) above ca. 49 Ma basaltic basement at International Ocean Discovery Program Site U1438 in the Amami Sankaku Basin. During deposition of Unit IV the site was located similar to 250 km from the plate edge, where Izu-Bonin-Mariana subduction initiated at 52 Ma. Basement basalts are overlain by a mudstone-dominated subunit (IVC) with a thin basal layer of dark brown metalliferous mudstone followed by mudstone with sparse, graded laminae of amphibole- and biotite-bearing tuffaceous sandstone and siltstone. Amphibole and zircon ages from these laminae suggest that the intermediate subduction-related magmatism that sourced them initiated at ca. 47 Ma soon after basement formation. Overlying volcaniclastic, sandy, gravity-flow deposits (subunit IVB) have a different provenance; shallow water fauna and tachylitic glass fragments indicate a source volcanic edifice that rose above the carbonate compensation depth and may have been emergent. Basaltic andesite intervals in upper subunit IVB have textures suggesting emplacement as intrusions into unconsolidated sediment on a volcanic center with geochemical and petrological characteristics of mafic, differentiated island arc magmatism. Distinctive Hf-Nd isotope characteristics similar to the least-radiogenic Izu-Bonin-Mariana boninites support a relatively old age for the basaltic andesites similar to detrital amphibole dated at 47 Ma. The absence of boninites at that time may have resulted from the position of Site U1438 at a greater distance from the plate edge. The upper interval of mudstone with tuffaceous beds (subunit IVA) progresses upsection into Unit III, part of a wedge of sediment fed by growing arc-axis volcanoes to the east. At Site U1438, in what was to become a reararc position, the succession of early extensional basaltic magmatism associated with spontaneous subduction initiation is followed by a rapid transition into potentially widespread subduction-related magmatism and sedimentation prior to the onset of focused magmatism and major arc building.
DOI10.1130/B35612.1
收录类别SCI
语种英语
资助项目National Science Foundation[OCE-1503694]; Ocean Leadership; Geological Society of America; Japan Agency for Marine-Earth Science and Technology; Japan Drilling Earth Science Consortium; National Natural Science Foundation of China[91958110]; National Natural Science Foundation of China[41473029]; Swiss National Science Foundation[P2LAP2_171819]; NSF[OCE 1537861]; NSF[1537135]; [25287133]
WOS研究方向Geology
WOS类目Geosciences, Multidisciplinary
WOS记录号WOS:000672732700005
出版者GEOLOGICAL SOC AMER, INC
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被引频次:9[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/175768
专题深海极端环境与生命过程研究中心
通讯作者Marsaglia, Kathleen M.
作者单位1.Calif State Univ Northridge, Dept Geol Sci, 18111 Nordhoff St, Northridge, CA 91330 USA
2.Univ South Carolina, Sch Earth Ocean & Environm, 701 Sumter St,EWSC617, Columbia, SC 29208 USA
3.Florida Int Univ, Earth & Environm Dept, AHC5-360, Miami, FL 33199 USA
4.Geol Survey Japan AIST, Cent 7 1-1-1 Higashi, Tsukuba, Ibaraki 3058567, Japan
5.Japan Agcy Marine Earth Sci & Technol JAMSTEC, 2-15 Natsushima Cho, Yokosuka, Kanagawa 2370061, Japan
6.Univ Lausanne, Inst Earth Sci, CH-1015 Lausanne, Switzerland
7.Univ Tasmania, Inst Marine & Antarctic Studies, Hobart, Tas 7004, Australia
8.Chinese Acad Sci, Ctr Deep Sea Res, Inst Oceanol, Qingdao 266071, Peoples R China
9.Univ Leeds, Sch Earth & Environm, Leeds LS2 9JT, W Yorkshire, England
10.Univ Tasmania, Sch Earth Sci, Hobart, Tas 7001, Australia
11.Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT 2601, Australia
12.Univ Western Australia, Sch Earth Sci, M004,35 Stirling Highway, Crawley, WA 6009, Australia
13.Indiana Univ Purdue Univ, Dept Earth Sci, Indianapolis, IN 46202 USA
14.Texas A&M Univ, Int Ocean Discovery Program, 1000 Discovery Dr, College Stn, TX 77845 USA
15.GEOMAR Helmholtz Ctr Ocean Res Kiel, Wischhofstr 1-3, D-24148 Kiel, Germany
16.CALTECH, Seismol Lab, Pasadena, CA 91125 USA
17.Chinese Acad Sci, Inst Oceanol, 7 Nanhai Rd, Qingdao 266071, Peoples R China
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Waldman, Ryan J.,Marsaglia, Kathleen M.,Hickey-Vargas, Rosemary,et al. Sedimentary and volcanic record of the nascent Izu-Bonin-Mariana arc from IODP Site U1438[J]. GEOLOGICAL SOCIETY OF AMERICA BULLETIN,2021,133(7-8):1421-1440.
APA Waldman, Ryan J..,Marsaglia, Kathleen M..,Hickey-Vargas, Rosemary.,Ishizuka, Osamu.,Johnson, Kyle E..,...&Jiang, Fuqing.(2021).Sedimentary and volcanic record of the nascent Izu-Bonin-Mariana arc from IODP Site U1438.GEOLOGICAL SOCIETY OF AMERICA BULLETIN,133(7-8),1421-1440.
MLA Waldman, Ryan J.,et al."Sedimentary and volcanic record of the nascent Izu-Bonin-Mariana arc from IODP Site U1438".GEOLOGICAL SOCIETY OF AMERICA BULLETIN 133.7-8(2021):1421-1440.
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