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期刊名称: Gondwana Research
Volume:29    Issue:1        Page:1-40
ISSN:1342-937X

Tectonic architecture and multiple orogeny of the Qinling Orogenic Belt, Central China期刊论文

作者: Dong Yunpeng Santosh M
DOI:10.1016/j.gr.2015.06.009

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页码: 1-40
被引频次: 173
出版者: Elsevier B.V,ELSEVIER SCIENCE BV
期刊名称: Gondwana Research
ISSN: 1342-937X
卷期: Volume:29    Issue:1
语言: English
摘要: The Qinling Orogenic Belt (QOB) is located between the North China and South China Blocks, and has been considered to have formed by the collision between these blocks. This contribution provides an overview of the composition, nature and ages of the principal tectonic elements including ophiolitic melanges and related volcanic rocks, gabbroic-granitic intrusions, metamorphic basement, sedimentary cover and its provenance in this orogen. The QOB represents a composite orogenic belt that witnessed four major episodes of accretion and collision between discrete continental blocks, such as the North China Block, North Qinling Block and the South China Block. The available geology, geochemistry and geochronology of these tectonic elements together with those of the adjacent regions, can be used to trace the polarity of the four stages of plate subduction, accretion, collision and the related tectonic history as follows. (1) The Grenvillian-aged orogeny along the Kuanping suture between the North Qinling Terrane and North China Block is associated with the southward subduction of Mesoproterozoic Ocean, which led to the amalgamation of the North Qinling Terrane and the North China Block at ca. 1.0 Ga. (2) The Neoproterozoic subduction/accretion as represented by the widely distributed terranes and volcanic-sedimentary rocks, resulted in a wide accretionary wedge formed by the southward accretion to the South China Block. (3) The Paleozoic orogeny along the Shangdan suture between the North and South Qinling Blocks is characterized by Early Paleozoic ocean-continent subduction and a long-lived Late Paleozoic continent-continent subduction. The polarity and detailed evolutionary process of the Early Paleozoic ocean-continent subduction have been constrained by the ophiolitic melange, island-arc related volcanics and intrusions in the North Qinling Belt, as well as the evolutionary history of the Erlangping back-arc basin. The northward subduction and destruction of the Shangdan Ocean during Early Devonian was succeeded by continent-continent subduction beneath the North Qinling Terrane from Middle Devonian to Early Triassic. (4) The Triassic collisional orogeny occurred between the South Qinling Block and South China Block along the Mianlue suture. Silurian rifting along the present Mianlue zone marks the precursor of the eastern Mianlue Ocean, which separated the South Qinling Block from the South China Block during Late Paleozoic. The northward subduction of the ocean led to the Middle Triassic collision between the South China Block and the South Qinling Block. (5) After the collision, the whole QOB evolved into an intra-continental orogen, including Early Jurassic differential tectonics, Late Jurassic to Early Cretaceous compression and thrusting, and Late Cretaceous to Paleogene orogen collapse and depression. These multiple orogenies resulted in abundant mineralization, the genetic types, spatial distribution and metallogenic epochs which correlate well with the tectonics and evolutionary history of the QOB. (C) 2015 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.
相关主题: Geochemistry, Geochronology, Multiple orogeny, Tectonic evolution, Qinling Orogenic Belt, YANGTZE BLOCK CONSTRAINTS, GA CONTINENTAL-CRUST, ZIRCON U-PB, COESITE-BEARING ECLOGITES, GEOSCIENCES, MULTIDISCIPLINARY, RADIATING DYKE SWARM, HF ISOTOPE GEOCHEMISTRY, FORMED MAFIC CRUST, PORPHYRY MO DEPOSIT, SOUTH CHINA, PRE-RODINIA SUPERCONTINENT, Ophiolites, Rocks, Sedimentary, Tectonics (Geology), Volcanic ash, tuff, etc,

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