全球前寒武纪基底构造格局与古大陆再造问题

王鸿祯; 张世红

Volume 27 Issue 5

Sep. 2002

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WANG Hong-zhen, ZHANG Shi-hong, 2002. Tectonic Pattern of the World Precambrian Basement and Problems of Paleocontinent Reconstruction. Earth Science, 27(5): 467-481.

Citation:

WANG Hong-zhen, ZHANG Shi-hong, 2002. Tectonic Pattern of the World Precambrian Basement and Problems of Paleocontinent Reconstruction. Earth Science, 27(5): 467-481.

WANG Hong-zhen, ZHANG Shi-hong, 2002. Tectonic Pattern of the World Precambrian Basement and Problems of Paleocontinent Reconstruction. Earth Science, 27(5): 467-481.

Citation:

WANG Hong-zhen, ZHANG Shi-hong, 2002. Tectonic Pattern of the World Precambrian Basement and Problems of Paleocontinent Reconstruction. Earth Science, 27(5): 467-481.

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Tectonic Pattern of the World Precambrian Basement and Problems of Paleocontinent Reconstruction

Faculty of Earth Sciences and Mineral Resources, China University of Geosciences, Beijing 100083, China

Received Date: 2002-07-21
Publish Date: 2002-09-25

Abstract

Abstract

The tectonic frame and subdivision of tectonic units of the world Precambrian basement are essential for paleocontinent reconstruction. In this paper, a three rank system of tectonic units, the first rank tectonic domain, the second rank craton (continental platform) or 'Region', and the third rank continental nucleus, massif and belt, is proposed, based mainly on situations in Neoproterozoic Jinning and the Early Mesozoic Indosinian epochs. Altogether 5 domains, 14 cratons or regions, and a number of nuclei, massifs and belts within and outside of the cratons that are related to or derived from the cratons, are distinguished and catalogued for further reference and improvement (Fig. 1, Table 1). We deem that a supercontinent is a constituent part of its contemporary pangea, and the present research of supercontinent Rodinia has entered into the study of its contemporary pangea, the Pangea-850 in our former use. In the early Neoproterozoic, the three Chinese cratons, Sino-Korean, Yangtzean, Tarimian and the Cathaysian Region, were probably partly collided with each other through the Jinningian orogeny, and were not very far from each other. We have called the combined entirety, including the Central Asian Karakum Massif, the Axial Asian or Cathaysianan Do-main. The current models for Rodinia, especially the SWEAT connection, are discussed. As the characteristic Neo-proterozoic (900-850 Ma) Qingbaikouan mega algae Chuaria-Tawuia assemblage were amply found both in Sino-Korea and Cathaysian in eastern Asia and in the Little Dal Group in western North America, we suggest the Axial Asian or Cathaysianan Domain may have been placed near the western margin of Laurentia, and the East Gondwanan cratons may on that account be shifted southwards (on map). Other problems including the orientation of the Siberian Craton and the Pan-African belts in the West Gondwanan Domain are also briefly noted. A refined reconstruction of the Middle Permian Epoch (280-257 Ma) for Pangea-250, the only recognized Pangea up to now, is presented, in which three marine biogeographical realms and constituent provinces based mainly on corals and brachiopods are subdi-vided. The signals for the four well known paleophytic realms, Angaran, Cathaysian, Euramerican and Gondwanan, and of some representative assemblages of the marine provinces are shown on Fig. 3, and their significance in paleo-continent reconstruction are briefly discussed.
- supercontinent,
- pangea,
- paleocontinent reconstruction,
- tectonic domain,
- axial Asian,
- Cathaysiana,
- biogeography,
- Jinningian orogenic epoch

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References(104)

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