准噶尔盆地腹部早二叠纪—晚石炭纪火山岩的构造背景分析

邵雨, 张顺存, 史基安, 支东明, 孙国强. 准噶尔盆地腹部早二叠纪—晚石炭纪火山岩的构造背景分析[J]. 地质科学, 2012, 47(4): 1005-1015.
引用本文: 邵雨, 张顺存, 史基安, 支东明, 孙国强. 准噶尔盆地腹部早二叠纪—晚石炭纪火山岩的构造背景分析[J]. 地质科学, 2012, 47(4): 1005-1015.
Shao Yu, Zhang Shuncun, Shi Ji'an, Zhi Dongming, Sun Guoqiang. Tectonic settings of the Late Carboniferous-Early Permian volcanic rocks,central Junggar Basin[J]. Chinese Journal of Geology, 2012, 47(4): 1005-1015.
Citation: Shao Yu, Zhang Shuncun, Shi Ji'an, Zhi Dongming, Sun Guoqiang. Tectonic settings of the Late Carboniferous-Early Permian volcanic rocks,central Junggar Basin[J]. Chinese Journal of Geology, 2012, 47(4): 1005-1015.

准噶尔盆地腹部早二叠纪—晚石炭纪火山岩的构造背景分析

详细信息
    通讯作者: 张顺存, 男, 1973年11月生, 博士, 副研究员, 储层地球化学与储层地质学专业。 E-mail: zhangshuncun@126.com
  • 中图分类号: P542; P618

Tectonic settings of the Late Carboniferous-Early Permian volcanic rocks,central Junggar Basin

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    Corresponding author: Zhang Shuncun
  • 从中生代到新生代,准噶尔盆地腹部地区连续沉积,缺少腹部地区的样品,因此准噶尔地区晚古生代构造演化的研究常集中于盆地周围的褶皱造山带。本文通过对早二叠纪—晚石炭纪钻井岩心样品的地球化学、岩石学特征进行研究。结果表明: 1)许多钻井的不同层位中,都发育着表明水上喷发环境的褐色凝灰岩; 2)准噶尔盆地腹部早二叠纪—晚石炭纪火山岩主要是碱性玄武岩、安山岩及少量的流纹岩,样品的大部分以高碱为特征,反映了喷发于陆上增厚地壳的构造背景; 3)岩心观察、薄片鉴定及主量和微量元素的分析结果表明,晚古生代准噶尔盆地腹部属于大陆构造背景。石炭系火山岩的底部也许存在许多的古老陆块基底。
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出版历程
收稿日期:  2012-05-26
修回日期:  2012-08-21
刊出日期:  2012-10-25

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