华北克拉通北缘早二叠世堆晶岩及其构造意义

邵济安; 田伟; 张吉衡

doi:10.3799/dqkx.2015.131

Volume 40 Issue 9

Sep. 2015

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Shao Ji'an, Tian Wei, Zhang Jiheng, 2015. Early Permian Cumulates in Northern Margin of North China Craton and Their Tectonic Significances. Earth Science, 40(9): 1441-1457. doi: 10.3799/dqkx.2015.131

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Shao Ji'an, Tian Wei, Zhang Jiheng, 2015. Early Permian Cumulates in Northern Margin of North China Craton and Their Tectonic Significances. Earth Science, 40(9): 1441-1457. doi: 10.3799/dqkx.2015.131

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Early Permian Cumulates in Northern Margin of North China Craton and Their Tectonic Significances

doi: 10.3799/dqkx.2015.131

Shao Ji'an^{1, 2
,},
Tian Wei^{1, 2},
Zhang Jiheng³

1.
Key Laboratory of Orogenic Belts and Crustal Evolution of the Ministry of Education, Peking University, Beijing 100871, China
2.
School of Earth and Space Sciences, Peking University, Beijing 100871, China
3.
Key Laboratory of Computational Geodynamics of Chinese Academy of Sciences; University of Chinese Academy of Sciences, Beijing 100049, China

Received Date: 2015-05-18
Publish Date: 2015-09-15

Abstract

Abstract

Understanding about genesis of the Early Permian basic-ultrabasic rocks in the northern margin of North China craton are varied, with one of the influential viewpoints suggesting that they are related with activities of "Andes-type continental margin", which is discussed in this paper based on researches of the cumulates in east Hebei Province. Early Permian basic-ultrabasic cumulates controlled by Fengning-Longhua lithospheric faults are distributed discontinuously in the northern margin of North China craton. The SHRIMP Zircon U-Pb ages from cumulates are 280-300 Ma. Petrographic studies confirm that the complexes consist of a suite of cumulates including dunite, pyroxenite, amphibolite, gabbro, diorite, anorthosite, and so on, which in turn can be further divided into layered and circular ones, both with obvious cumulate texture. Mineralogical studies show that hornblende, pyroxene, and phlogolite in cumulates all are characterized by mantle sourced components of high Mg and high Cr. Sr/Ba ratio of cumulates with different components does not change with their melting degrees, showing that cumulates possess a fractional crystallization trend. Similar REE patterns and transition group elements reveal their consanguinity. Comparison of cumulates of the Late Paleozoic with those of the Early Mesozoic from the concerned area indicates that these Early Permian cumulates have characteristics of an initial-rift magma, which offers the earliest evidence of the transformation from the stable to the active one of continental crust of North China craton. Viewed from broader regions, activities of this period in this area are driven by deeper geodynamics.
- northern margin of North China craton,
- Early Permian,
- cumulate,
- crust-mantle transition zone,
- extensional background,
- tectonics

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