来宾地区中晚二叠世之交碳同位素负漂及其意义

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• 论文作者：邱振 ; 王清晨 ; 邹才能 ; 严德天 ; 侯连华
• 年：2013
• 作者机构：中国石油勘探开发研究院;中国科学院地质与地球物理研究所;中国地质大学;
• 会议召开时间：2013-04-16
• 会议录名称：第一届全国青年地质大会论文集
• 语种：中文
• 分类号：P597;P534.46
• 学会代码：DXHD
• 会议名称：第一届全国青年地质大会
• 会议地点：中国福建福州
• 主办单位：中国地质学会青年工作委员会
• 学会名称：中国地质学会地质学报编辑部
• 页数：4
• 文件大小：856k
• 原文格式：O
• 会议级别：全国

摘要

<正>中晚二叠世之交,发生了一系列全球性重要事件,如中二叠世末的全球规模的海平面下降和生物灭绝(又称瓜德鲁普末生物灭绝)及峨眉山玄武岩喷发事件。前人对这一时期的碳酸盐岩碳同位素(δ~(13)C_(carb))研究已开展不少工作,并取得了许多成果,如我国扬子台地的δ~(13)C_(carb)负漂>5‰,被认为与峨眉山玄武岩喷发具有密切联系(Wignall et al.,2009a;Bond et al.,2010a),以及日本Kamura地区中二叠世晚期的δ~(13)C_(carb)正漂,即Kamura事件,被解

引文

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