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华北克拉通太古宙典型地区栖霞县幅1:5万地质图修编——野外地质调查和SHRIMP锆石U-Pb定年

万渝生 刘敦一 宋志勇 王来明 颉颃强 刘守偈 侯建华 董春艳 谢士稳 白文倩

地质通报2017,Vol.36Issue(11):1927-1941,15.
地质通报2017,Vol.36Issue(11):1927-1941,15.

华北克拉通太古宙典型地区栖霞县幅1:5万地质图修编——野外地质调查和SHRIMP锆石U-Pb定年

Early Precambrian evo-lution of the Qixia area, eastern North China Craton: Evidence from geological mapping and SHRIMP U-Pb zircon dating

万渝生 1刘敦一 1宋志勇 2王来明 2颉颃强 1刘守偈 1侯建华 2董春艳 1谢士稳 1白文倩1

作者信息

  • 1. 中国地质科学院地质研究所北京离子探针中心,北京100037
  • 2. 山东省地质调查院,山东济南250013
  • 折叠

摘要

Abstract

Qixia is a typical area of Early Precambrian basement in eastern Shandong, North China Craton. Many TTG rocks were once considered to be supracrustal rocks (the Jiaodong Group), and the formation ages of the rocks have only been determined in a few outcrops in the original geological map (1:50000) of the area. In this study, the authors carried out geological mapping and SHRIMP U-Pb zircon dating on more than 30 samples in order to determine the temporal and spatial distribution of the TTG rocks. In the newly compiled geological map (1:50000), the main rock types of the Archean basement are tonalite gneisses with ages~2.9Ga, ~2.7Ga and ~2.5Ga and some local trondhjemite gneisses of the same ages. Supracrustal rocks of ~2.9Ga and ~2.5Ga (the Huangyadi supracrustal rocks and the Jiaodong Group) are very rare. All of the rocks roughly extend in a NWW-SEE direction, probably as a result of the strong late Neoarchean and late Paleoproterozoic tectonothermal events.

关键词

胶东/TTG/太古宙/地质填图/SHRIMP锆石U-Pb定年

Key words

eastern Shandong/TTG/Archean/geological mapping/SHRIMP zircon U-Pb dating

分类

天文与地球科学

引用本文复制引用

万渝生,刘敦一,宋志勇,王来明,颉颃强,刘守偈,侯建华,董春艳,谢士稳,白文倩..华北克拉通太古宙典型地区栖霞县幅1:5万地质图修编——野外地质调查和SHRIMP锆石U-Pb定年[J].地质通报,2017,36(11):1927-1941,15.

基金项目

中国地质调查局项目《华北克拉通东部古陆块的形成演化及立典地区1:5万专题填图》(编号:DD20160121-03和《中国太古宙地壳形成与演化综合研究》(编号:121201102000150012) (编号:DD20160121-03和《中国太古宙地壳形成与演化综合研究》(编号:121201102000150012)

地质通报

OA北大核心CSCDCSTPCD

1671-2552

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