首页|冀西北地区中侏罗世玄武岩的首次发现及其地质意义

冀西北地区中侏罗世玄武岩的首次发现及其地质意义

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笔者等在张家口市宣化区—涿鹿县一带中—上侏罗统髫髻山组底部首次发现玄武岩组合,其时代归属、地球化学性质及地质意义需要开展研究.本文对玄武岩开展地质学、岩石学、地球化学和同位素年代学研究.玄武岩Si02含量为39.49%~49.74%,Mg#为28~65,里特曼指数σ主要为2.61~33.12.玄武岩获得LA-ICP-MS锆石U-Pb年龄为164.3±2.6Ma,时代为中侏罗世,代表髫髻山组底界年龄.玄武岩属于碱性玄武岩系列,与上覆粗面岩构成双峰式火山岩组合,表明髫髻山组早期火山岩形成于大陆板内拉张环境.该套玄武岩是髫髻山组中性火山岩的玄武质岩浆底侵作用的地质学、岩石学和大地构造学证据.
The first discovery of Middle Jurassic basalts in Northwestern Hebei Province and its geological significance
This paper is the result of geological survey.Writers first discovered the basalt association at the bottom of the Middle—Upper Jurassic Tiaojishan Formation in the Xuanhua District—Zhuolu County area,Zhangjiakou City,whose age,geochemical properties,and geological significance requires to further research.This article conducts geological,petrological,geochemical,and isotopic chronological studies on the basalts.The SiO2 content of the basalt ranges from 39.49%to 49.74%,Mg # ranges from 28 to 65,and the Rittmann index(σ)ranging from 2.61 to 33.12.The basalt belongs to the alkaline basalt series and forms bimodal volcanic rock combination with the overlying trachyte,indicating that the early volcanic rocks of the Tiaojishan Formation were formed in a continental plate tensile environment.This set of basalts is a geological,petrological,and tectonic study of the basaltic magma underplating of the neutral volcanic rocks of the Tiaojishan Formation.

northwestern HebeiMiddle Jurassic basaltsTiaojishan Formationplate tension

白春东、许凡、李泽阳、孟家葆、朱本鸿

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河北省区域地质调查院,河北廊坊,065000

冀西北 中侏罗世玄武岩 髫髻山组 底侵作用 板内拉张

河北省自然资源厅项目

2024

地质论评
中国地质学会

地质论评

CSTPCD北大核心
影响因子:1.842
ISSN:0371-5736
年,卷(期):2024.70(3)
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