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利用沉积地球化学特征分析古环境及海平面变化——以鲁西东部中下寒武统为例
引用本文:张国仁.利用沉积地球化学特征分析古环境及海平面变化——以鲁西东部中下寒武统为例[J].国土资源,1997(1).
作者姓名:张国仁
作者单位:地质矿产部辽宁地质矿产勘查开发局区域地质调查队
摘    要:过对鲁西东部中下寒武统研究表明:利用δ13C和δ18O以及Sr,Ni,V,Ba,B元素地球化学特征,不仅可以判断沉积古气候、古盐度、古水温、氧化-还原条件,而且还能提供海平面变化旋回及暴露-间断面确立的依据。研究证明此方法是非常有效的。

关 键 词:碳、氧同位素NiSrBaVB  古环境  海平面变化  沉积地球化学

GEOLOGICAL CHARACTERISTICS AND EMPLACEMENT MECHANISM OF CALEDONIAN INTRUSIVE ROCKS IN JIANP ING,LIAONING
Chen Shuiang Gao Shirong Li Suxia.GEOLOGICAL CHARACTERISTICS AND EMPLACEMENT MECHANISM OF CALEDONIAN INTRUSIVE ROCKS IN JIANP ING,LIAONING[J].Land & Resources,1997(1).
Authors:Chen Shuiang Gao Shirong Li Suxia
Abstract:The Caledonian intrusive rocks in Jianping emplaced in the early stage of Caledonian,which the U-P concordant ages is 573.9Ma.According to rock lineage unit subdivision criterion,the intrusive rocks from early to late successively can be divided into Shanggou-unit diorite,Zhoujiatai-unit quartz diorite,Fangshen-unit granodiorite,Yangpo-unit granite,all these units belonging to Shangmajiazi ultra-unit.The genisis type is I-type and the material came from the lower crust.The emplacement mechanism is ballon-expansion style.Owing to the multiphase pulsating intrusion,the struction is a complete.
Keywords:Shangmajiazi Ultra-unit I-type Ballon-expansion style  
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