Expedition 357 summary

Expedition 357 summary
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远征357概要

DOI:
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发表时间:
2017
期刊:
影响因子:
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通讯作者:
R. Zhao
R. Zhao
中科院分区:
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文献类型:
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作者:
G. Früh;B. Orcutt;S. Green;C. Cotterill;S. Morgan;N. Akizawa;G. Bayrakci;J. Behrmann;C. Boschi;W. J. Brazleton;M. Cannat;K. Dunkel;J. Escartín;M. Harris;E. Herrero;K. Hesse;B. John;S. Lang;M. Lilley;H. Liu;L. Mayhew;A. McCaig;B. Ménez;Y. Morono;M. Quéméneur;S. Rouméjon;A. Ratnayake;M. Schrenk;E. Schwarzenbach;K. I. Twing;D. Weis;S. A. Whattham;M. Williams;R. Zhao

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International Ocean Discovery Program (IODP) Expedition 357 successfully cored an east–west transect across the southern wall of Atlantis Massif on the western flank of the Mid-Atlantic Ridge (MAR) to study the links between serpentinization processes and microbial activity in the shallow subsurface of highly altered ultra- mafic and mafic sequences that have been uplifted to the seafloor along a major detachment fault zone. The primary goals of this ex- pedition were to (1) examine the role of serpentinization in driving hydrothermal systems, sustaining microbial communities, and se- questering carbon; (2) characterize the tectonomagmatic processes that lead to lithospheric heterogeneities and detachment faulting; and (3) assess how abiotic and biotic processes change with varia- tions in rock type and progressive exposure on the seafloor. To ac- complish these objectives, we developed a coring and sampling strategy centered on the use of seabed drills—the first time that such systems have been used in the scientific ocean drilling pro- grams. This technology was chosen in the hope of achieving high recovery of the carbonate cap sequences and intact contact and de- formation relationships. The expedition plans also included several engineering developments to assess geochemical parameters during drilling; sample bottom water before, during, and after drilling; sup- ply synthetic tracers during drilling for contamination assessment; acquire in situ electrical resistivity and magnetic susceptibility mea- surements for assessing fractures, fluid flow, and extent of ser- pentinization; and seal boreholes to provide opportunities for future experiments. (...)
DOI: 10.1130/g23657a.1
发表时间: 2007-10-01
期刊: GEOLOGY
影响因子: 5.8
作者:
McCaig, Andrew M.;Cliff, Robert A.;MacLeod, Christopher J.
通讯作者: MacLeod, Christopher J.
DOI: 10.1016/j.lithos.2008.10.022
发表时间: 2009-09-01
期刊: LITHOS
影响因子: 3.5
作者:
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通讯作者: Klein, Frieder
DOI: 10.1016/j.epsl.2009.08.007
发表时间: 2009-09-30
影响因子: 5.3
作者:
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通讯作者: Searle, R. C.