A HIMU-Like Endmember Hiding in the Turkana Depression Continental Lithospheric Mantle

IF 2.9 2区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Andrew R. Bollinger, Tyrone O. Rooney, Eric L. Brown, Frank C. Ramos
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Abstract

The fate of continental lithosphere during rifting is central to the process of continental extension. The continental lithospheric mantle comprises both depleted and enriched domains that may contribute to magma generation during extension. The East African Rift System is the archetypal example of a magma-rich continental rift, with the Turkana Depression containing the most extensive temporal record of mafic magmatism. There is debate as to the contribution of continental lithosphere to this mafic magmatism, with suggestions that HIMU-like isotopic signatures, often attributed to the continental lithosphere, are derived instead from a heterogeneous mantle plume. We focus on Miocene lavas that are characterized by radiogenic 206Pb/204Pb > 19.3, requiring a contribution from an HIMU-like endmember in their origin. We present a novel two-stage chromatographic metasomatism model that demonstrates that a HIMU-like endmember can be generated through time-integrated evolution within the continental lithospheric mantle. The first model stage uses an initial composition for the metasomatizing agent equivalent to a subduction magma to generate metasomes within the continental lithosphere during the Pan-African stabilization of the regional lithosphere (∼700 Ma). During Mesozoic rifting, the second model stage simulates destabilization and melting of these initial metasomes, re-enriching the surrounding lithosphere to generate new Mesozoic metasomes. Melts of these metasomes, when combined with melts of the regional asthenosphere, are consistent with the observed trace element and isotopic signatures of Turkana Miocene lavas. These findings suggest an important role for the continental lithospheric mantle during rifting and obviate the need for a complex, heterogenous plume.

Abstract Image

隐藏在图尔卡纳坳陷大陆岩石圈地幔中的himu状端元
大陆岩石圈在裂陷过程中的命运是大陆伸展过程的核心。大陆岩石圈地幔包括贫域和富域,可能在伸展过程中产生岩浆。东非裂谷系是岩浆丰富的大陆裂谷的典型例子,图尔卡纳坳陷包含了最广泛的岩浆活动的时间记录。关于大陆岩石圈对这种岩浆活动的贡献存在争议,有人认为,通常归因于大陆岩石圈的类似himu的同位素特征来源于非均质地幔柱。中新世火山岩以放射性成因206Pb/204Pb >;19.3,在其起源中需要一个类似于himu的端元的贡献。我们提出了一种新的两阶段色谱交代模型,该模型表明,在大陆岩石圈地幔内,通过时间积分演化可以产生一个类似于himu的端元。在区域岩石圈泛非稳定时期(~ 700 Ma),第一个模式阶段使用相当于俯冲岩浆的交代剂的初始成分在大陆岩石圈内产生交代体。在中生代裂谷期,第二阶段模拟了这些初始交代体的失稳和熔融作用,使周围岩石圈重新富集生成新的中生代交代体。这些交代体的熔体与区域软流圈熔体相结合,与图尔卡纳中新世熔岩的微量元素和同位素特征一致。这些发现表明,大陆岩石圈地幔在裂谷过程中起着重要作用,并消除了对复杂的非均质地幔柱的需要。
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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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