Metamorphism of basement rocks in the Central Zone of the North China Craton: implications for Paleoproterozoic tectonic evolution

G C Zhao, Peter Anthony Cawood, S A Wilde, S Min, L Z Lu

Research output: Contribution to journalReview articlepeer-review

612 Citations (Scopus)

Abstract

Lithological, structural, metamorphic and geochronological data for the North China Craton enable its division into the Western and Eastern Blocks of Archean to Paleoproterozoic age separated by a north-south trending Paleoproterozoic orogenic belt: the Central Zone. The Central Zone is divisible into a series of low- to medium-grade granite-greenstone belts and high-grade metamorphic terrains containing reworked Archean material and late Archean to Paleoproterozoic juvenile igneous and sedimentary rocks which developed in intra-continental magmatic are and intra-arc basin environments bordering the western margin of the Eastern Block. The basement rocks from the Central Zone, regardless of their protolith age, composition and metamorphic grade, record a metamorphic history characterized by nearly isothermal decompression (M-2) and then retrogressive cooling (M-3) following peak metamorphism (M-1). The decompression textures are represented by worm-like hypersthene + plagioclase symplectites or clinopyroxene + orthopyroxene + plagioclase coronas in mafic granulites, hornblende/cummingtonite + plagioclase symplectites in amphibolites, and cordierite coronas and cordierite + orthopyroxene or cordierite + spinel symplectites in pelitic rocks. The cooling textures are shown by hornblende + plagioclase symplectites in mafic granulites, chlorite + epidote + mica retrogressive rims around garnet or hornblende grains in amphibolites, and biotite + K-feldspar +/- muscovite +/- magnetite replacing garnet, cordierite and sillimanite in pelitic gneisses. These textural relations and their P-T estimates define near-isothermal decompressional clockwise P-T paths, which, in combination with lithological, structural and geochronological constraints, are in accord with collision between the Eastern and Western Blocks of the North China Craton at similar to 1.8 Ga. (C) 2000 Elsevier Science B.V. All rights reserved.

Original languageEnglish
Pages (from-to)55-88
Number of pages34
JournalPrecambrian Research
Volume103
Issue number1-2
DOIs
Publication statusPublished - Sept 2000

Keywords

  • continental collision
  • metamorphism
  • North China Craton
  • P-T paths
  • tectonothermal evolution
  • TEMPERATURE-TIME PATHS
  • CONSISTENT THERMODYNAMIC DATA
  • HIGH-GRADE ROCKS
  • T-T PATHS
  • REGIONAL METAMORPHISM
  • CONTINENTAL-CRUST
  • LIAONING PROVINCE
  • INNER-MONGOLIA
  • PELITIC ROCKS
  • GARNET

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