Paleoproterozoic Multistage Metamorphic Ages Registered in the Precambrian Basement Rocks at the Southeastern Margin of the North China Craton and Their Geological Implications

The Precambrian basement rocks in the Bengbu and neighboring areas, located at the southeastern margin of the North China Craton, occur as granulite terrains and xenoliths in the Mesozoic dioritic porphyry.

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Veröffentlicht in:Acta geologica Sinica (Beijing) 2016-12, Vol.90 (6), p.2265-2266
Hauptverfasser: LIU, Yican, ZHANG, Pingang, WANG, Chengcheng, NIE, Jiazhen
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container_title Acta geologica Sinica (Beijing)
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creator LIU, Yican
ZHANG, Pingang
WANG, Chengcheng
NIE, Jiazhen
description The Precambrian basement rocks in the Bengbu and neighboring areas, located at the southeastern margin of the North China Craton, occur as granulite terrains and xenoliths in the Mesozoic dioritic porphyry.
doi_str_mv 10.1111/1755-6724.13038
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subjects 中国北方
克拉通
前寒武纪
南缘
变质年龄
古元古代
地质意义
基底岩石
title Paleoproterozoic Multistage Metamorphic Ages Registered in the Precambrian Basement Rocks at the Southeastern Margin of the North China Craton and Their Geological Implications
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