Metasomatism and Melting of Cordilleran Lithosphere Resulting From Sediment Relamination During Shallow Subduction

IF 2.9 2区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
C. D. Hiett, D. L. Newell, J. W. Shervais
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引用次数: 0

Abstract

Mantle xenoliths recovered from the modern backarc region of the northern Altiplano Plateau record metasomatism by slab-derived silicic melts, and a suite of Quaternary volcanics suggest that melting of accreted crustal material has persisted since shallow subduction in the Oligocene. Xenoliths recovered from a suite of high-K andesitic lava flows include phlogopite- and calcite-rich orthopyroxenites and harzburgites, a wehrlite, and a phlogopite schist. Xenolith hosted calcite yields δ13C and δ18O values of −2.49 to +0.77‰ VPDB and +15.8 to +16.4‰ VSMOW, respectively, reflecting inputs of subducted marine carbonates in the metasomatizing melt. Arc-like trace element patterns and 87Sr/86Sr ratios further support a subduction influence. Major and trace element characteristics of Quaternary potassic basalts and intermediate alkaline lavas, with the presence of mantle xenoliths, contradict magmatic differentiation or mixing models to yield intermediate composition melts. Instead, we suggest that intermediate composition lavas are derived from the melting of sediments accreted to the base of the continental lithosphere during shallow subduction in the late Eocene-Oligocene. Melting of accreted material produces silicic alkaline melts, which react with peridotite to produce alkaline basaltic melts and residual phlogopite-orthopyroxenites. These processes explain the observed xenolith suite and local high-K basaltic volcanism, and the intermediate lavas may represent sediment melts that ascended to the surface minimally altered by exploiting the Cusco-Vilconata fault system. These observations inform mass transfers during shallow subduction and melting and metasomatism in the lithospheric mantle, with implications for the generation of alkaline magmatism and rheologic weakening in cordilleran regions globally.

Abstract Image

浅俯冲过程中沉积物再分层引起的科迪勒拉岩石圈的交代和熔融作用
从高原北部现代弧后地区恢复的地幔捕虏体记录了板块衍生的硅熔体的交代作用,以及一套第四纪火山岩表明,自渐新世浅俯冲以来,积累的地壳物质一直在熔融。从一套高钾安山岩熔岩流中发现的捕虏体包括富辉云母和方解石的直辉长石和黑子长石,一种辉长石和一种辉云母片岩。捕虏体方解石的δ13C和δ18O值分别为- 2.49 ~ +0.77‰VPDB和+15.8 ~ +16.4‰VSMOW,反映了交代熔体中俯冲海相碳酸盐的输入。弧状微量元素模式和87Sr/86Sr比值进一步支持俯冲作用的影响。第四纪钾质玄武岩和中碱性熔岩的主微量元素特征与地幔捕虏体的存在相矛盾,与岩浆分异或混合模式相矛盾,产生了中间成分熔体。相反,我们认为中间成分熔岩是在晚始新世-渐新世浅层俯冲过程中沉积到大陆岩石圈底部的沉积物熔融形成的。堆积物熔融生成硅碱性熔体,与橄榄岩反应生成碱性玄武岩熔体和残余辉绿-正辉石岩。这些过程解释了观测到的包体套件和局部高钾玄武岩火山作用,而中间熔岩可能代表了通过利用Cusco-Vilconata断裂系统而最小程度改变的上升到地表的沉积物熔体。这些观测结果揭示了岩石圈地幔在浅俯冲、熔融和交代过程中的质量传递,对全球科迪勒山脉地区碱性岩浆活动的产生和流变减弱具有启示意义。
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来源期刊
Geochemistry Geophysics Geosystems
Geochemistry Geophysics Geosystems 地学-地球化学与地球物理
CiteScore
5.90
自引率
11.40%
发文量
252
审稿时长
1 months
期刊介绍: Geochemistry, Geophysics, Geosystems (G3) publishes research papers on Earth and planetary processes with a focus on understanding the Earth as a system. Observational, experimental, and theoretical investigations of the solid Earth, hydrosphere, atmosphere, biosphere, and solar system at all spatial and temporal scales are welcome. Articles should be of broad interest, and interdisciplinary approaches are encouraged. Areas of interest for this peer-reviewed journal include, but are not limited to: The physics and chemistry of the Earth, including its structure, composition, physical properties, dynamics, and evolution Principles and applications of geochemical proxies to studies of Earth history The physical properties, composition, and temporal evolution of the Earth''s major reservoirs and the coupling between them The dynamics of geochemical and biogeochemical cycles at all spatial and temporal scales Physical and cosmochemical constraints on the composition, origin, and evolution of the Earth and other terrestrial planets The chemistry and physics of solar system materials that are relevant to the formation, evolution, and current state of the Earth and the planets Advances in modeling, observation, and experimentation that are of widespread interest in the geosciences.
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