蛇绿混杂岩就位机制及其大地构造意义新解:基于残余洋盆型蛇绿混杂岩构造解析的启示

王国灿; 张攀

doi:10.3799/dqkx.2019.056

Volume 44 Issue 5

May 2019

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Article Navigation > Earth Science > 2019 > 44(5): 1688-1704

Wang Guocan, Zhang Pan, 2019. A New Understanding on the Emplacement of Ophiolitic Mélanges and Its Tectonic Significance: Insights from the Structural Analysis of the Remnant Oceanic Basin-Type Ophiolitic Mélanges. Earth Science, 44(5): 1688-1704. doi: 10.3799/dqkx.2019.056

Citation:

Wang Guocan, Zhang Pan, 2019. A New Understanding on the Emplacement of Ophiolitic Mélanges and Its Tectonic Significance: Insights from the Structural Analysis of the Remnant Oceanic Basin-Type Ophiolitic Mélanges. Earth Science, 44(5): 1688-1704. doi: 10.3799/dqkx.2019.056

Citation:

Wang Guocan, Zhang Pan, 2019. A New Understanding on the Emplacement of Ophiolitic Mélanges and Its Tectonic Significance: Insights from the Structural Analysis of the Remnant Oceanic Basin-Type Ophiolitic Mélanges. Earth Science, 44(5): 1688-1704. doi: 10.3799/dqkx.2019.056

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A New Understanding on the Emplacement of Ophiolitic Mélanges and Its Tectonic Significance: Insights from the Structural Analysis of the Remnant Oceanic Basin-Type Ophiolitic Mélanges

doi: 10.3799/dqkx.2019.056

Wang Guocan^{1,2
,
,},
Zhang Pan¹

1.
Center for Global Tectonics, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
Geological Survey, China University of Geosciences, Wuhan 430074, China

Received Date: 2019-01-30
Publish Date: 2019-05-15

Abstract

Abstract

Ophiolites represent on-land fragments of paleo-oceanic crust and have been recognized as one of the key markers of suture zones. Here, we provide new insights into the emplacement of ophiolitic mélanges based on detailed geological mapping and structural analysis in the West Junggar and Songpan-Ganzi orogens. The results show that some ophiolitic mélange belts cannot be regarded as suture zones. The distribution of these ophiolitic mélange belts are usually associated with the structural processes during the closure of remnant oceanic basins. After the remnant oceanic basin is filled with thick clastic deposit, the oceanic lithosphere material as the base of the remnant basin can be injected into the overlying sedimentary strata through various faultings under the regional compressive stress, forming the remnant oceanic basin-type ophiolitic mélange system with dispersive distribution characteristics. Combining with previous researches, the emplacement mechanism of suture-zone type ophiolitic mélanges can be divided into three categories:subduction type, obduction type, and collision type.These different types of ophiolitic mélange belts will be superimposed and even re-emplaced by the tectonic processes of post-plate convergence, complicating their distribution. Therefore, identifying the ophiolitic mélanges formed in different tectonic processes and their backgrounds is of importance for understanding the process of ocean-continental transition and the tectonic evolution of orogenic belts.
- ophiolitic mélange,
- emplacement,
- remnant-oceanic basin,
- orogen,
- tectonics

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References(100)

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A New Understanding on the Emplacement of Ophiolitic Mélanges and Its Tectonic Significance: Insights from the Structural Analysis of the Remnant Oceanic Basin-Type Ophiolitic Mélanges

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