气候变化领域集成服务门户(CCPortal): The role of serpentinization and magmatism in the formation of decoupling interfaces at magma-poor rifted margins

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DOI	10.1016/j.earscirev.2019.102882
	The role of serpentinization and magmatism in the formation of decoupling interfaces at magma-poor rifted margins
	Gillard M.; Tugend J.; Müntener O.; Manatschal G.; Karner G.D.; Autin J.; Sauter D.; Figueredo P.H.; Ulrich M.
发表日期	2019
ISSN	0012-8921
卷号	196
英文摘要	In spite of recent progress in the understanding of magma-poor rifted margins, the processes leading to the formation and evolution of the exhumed mantle domain and its transition toward steady state oceanic crust remain debated. In particular, the parameters controlling the progressive localization of extensional deformation and magmatic processes leading to the formation of an oceanic spreading center are poorly understood. In this paper, we highlight the occurrence of two major decoupling horizons controlling the structural and magmatic evolution of distal magma-poor rifted margins. They are marked by strong seismic reflectors located at about 1 s TWTT (Upper Reflectors–UR) and 2 s TWTT (Lower Reflectors–LR) below top basement in domains of exhumed mantle at several magma-poor rifted margins. Both reflection seismic observations and studies on the physical properties of serpentinized mantle suggest that the UR likely results from deformation localized along a rheological interface at about 3 km below top basement, associated with an abrupt change in the mechanical behavior of peridotites once they are serpentinized to ~15%. We suggest that this interface played a major role in successive fault re-organizations during formation of the exhumed mantle domain. The comparison of reflection seismic observations with Alpine field analogues suggests that the LR likely results from an interaction between magmatism, deformation and hydration reactions during final rifting. Based on our results, we suggest that during final rifting the strain distribution is controlled first by hydration and then by magmatic processes in the domain of exhumed mantle. © 2019 Elsevier B.V.
英文关键词	Decoupling; Magma-poor margins; Seismic interpretation; Serpentinization
语种	英语
scopus关键词	deformation; magma; magmatism; oceanic crust; peridotite; rheology; rift zone; seismic reflection; seismicity; serpentinization; spreading center
来源期刊	EARTH-SCIENCE REVIEWS
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/209849
作者单位	Institut de Physique du Globe de Strasbourg, UMR7516, Université de Strasbourg/EOST, CNRS, 1 rue Blessig, Cedex, Strasbourg, F-67084, France; Sorbonne Université, CNRS-INSU, Institut des Sciences de la Terre Paris, ISTeP UMR 7193, Paris, F-75005, France; Total SA, R&D Department CSTJF, Pau, France; Institute of Earth Sciences, University of Lausanne, Géopolis, Lausanne, CH-1015, Switzerland; ExxonMobil Upstream Integrated Solutions Company, Global Tectonics & Structure, 22777 Springwoods Village Parkway, Spring, TX, United States
推荐引用方式 GB/T 7714	Gillard M.,Tugend J.,Müntener O.,et al. The role of serpentinization and magmatism in the formation of decoupling interfaces at magma-poor rifted margins[J],2019,196.
APA	Gillard M..,Tugend J..,Müntener O..,Manatschal G..,Karner G.D..,...&Ulrich M..(2019).The role of serpentinization and magmatism in the formation of decoupling interfaces at magma-poor rifted margins.EARTH-SCIENCE REVIEWS,196.
MLA	Gillard M.,et al."The role of serpentinization and magmatism in the formation of decoupling interfaces at magma-poor rifted margins".EARTH-SCIENCE REVIEWS 196(2019).