造山带橄榄岩岩石学与构造过程:以松树沟橄榄岩为例

张宏福; 于红

doi:10.3799/dqkx.2019.952

Volume 44 Issue 4

Apr. 2019

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Zhang Hongfu, Yu Hong, 2019. Petrological and Tectonic Evolution of Orogenic Peridotite Massif: A Case of Songshugou Peridotites. Earth Science, 44(4): 1057-1066. doi: 10.3799/dqkx.2019.952

Citation:

Zhang Hongfu, Yu Hong, 2019. Petrological and Tectonic Evolution of Orogenic Peridotite Massif: A Case of Songshugou Peridotites. Earth Science, 44(4): 1057-1066. doi: 10.3799/dqkx.2019.952

Zhang Hongfu, Yu Hong, 2019. Petrological and Tectonic Evolution of Orogenic Peridotite Massif: A Case of Songshugou Peridotites. Earth Science, 44(4): 1057-1066. doi: 10.3799/dqkx.2019.952

Citation:

Zhang Hongfu, Yu Hong, 2019. Petrological and Tectonic Evolution of Orogenic Peridotite Massif: A Case of Songshugou Peridotites. Earth Science, 44(4): 1057-1066. doi: 10.3799/dqkx.2019.952

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Petrological and Tectonic Evolution of Orogenic Peridotite Massif: A Case of Songshugou Peridotites

doi: 10.3799/dqkx.2019.952

Zhang Hongfu^1
,,
Yu Hong²

1.
State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an 710069, China
2.
State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

Received Date: 2018-09-23
Publish Date: 2019-04-15

Abstract

Abstract

Orogenic peridotite is one of major research targets not only for mantle geochemistry, but also for the formation and evolution of the orogenic belts. There are mainly three types of orogenic peridotites: (1) Alpine peridotite, i. e. lithospheric mantle tectonic-thermal diaper into the shallow orogenic crust; (2) mafic-ultramafic cumulates of layered intrusions underwent subduction and metamorphism; (3) ophiolitic peridotite.Detailed petrological and geochemical investigation on Songshugou mylonitized peridotites and their related high-grade metamorphic rocks demonstrates that the Songshugou peridotites recorded the whole cycle from the formation of an oceanic lithosphere to amphibolite-facies retrograde metamorphism. i. e. dunites produced during the formation of an oceanic lithosphere at 1 000-800 Ma; followed by the period of oceanic-continental transition during < 800-500 Ma, lithospheric dunites metasomatized to produce an amounts of metasomatic harzburgites; rapid deep subdution and eclogite-facies metamorphism at 500-480 Ma; and amphibolite-facies retrograde metasomatism during slow exhumation at 460-335 Ma, magnesium-rich anthophyllites in Songshugou peridotites, including tremolite, actinolite, and magnesium amphibole, were emerged at this stage.Thus it can be seen that ophiolitic orogenic peridotites can record the whole cycle from the orogen formation and its evolution.They often underwent four stages:(1) formation of an oceanic lithosphere (ophiolite) to produce dunites; (2) the period of oceanic-continental transition and the formation of metasomatic harzburgite due to mantle metasomatism; (3) deep lithosphere subduction and eclogite-facies metamorphism; (4) retrograde metamorphism when exhumed to the depth of amphibolite-facies, lots of anthophyllites in peridotites emerged in this stage. Different orogens may have a diverse rock types just in the depth of the deep subduction and in degrees of retrograde metamorphism. Finally, the age formation of ophiolites must be emphasized.Meantime, the high grade metamorphosed rocks can be completely destroyed due to the later retrograde metamorphism, this deserves a great attention.
- orogenic peridotite,
- metasomatic harzburgite,
- deep lithosphere subduction,
- amphibolite-facies retrograde metamorphism,
- ophiolite,
- petrology

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References(46)

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Petrological and Tectonic Evolution of Orogenic Peridotite Massif: A Case of Songshugou Peridotites

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