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  5. The Upper Ordovician Carbon and Strontium Isotopic Chemostratigraphy in Dawangou Section at Keping,N

The Upper Ordovician Carbon and Strontium Isotopic Chemostratigraphy in Dawangou Section at Keping,N

来源 :The International Conference of Gas Geochemistry (ICGG)(第13届 | 被引量 : 0次 | 上传用户：wysnl2009
【摘 要】
：
　　The Upper Ordovician is marked by two major global δ13C excursions,the older one is referred to as the Guttenberg carbon isotope excursion(GICE)and the you
【作 者】
：
HouMingcai;LiuXinchun;ChangXiaoling;DengMin;XingFengcun; 
【机 构】
：
State key laboratory of oil and gas reservoir geology and exploitation,Chengdu University of Technol
【出 处】
：
The International Conference of Gas Geochemistry (ICGG)(第13届
【发表日期】
：
2015年期
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　　The Upper Ordovician is marked by two major global δ13C excursions,the older one is referred to as the Guttenberg carbon isotope excursion(GICE)and the younger one is known as the Hirnantian carbon isotope excursion(HICE); they have been observed in South America,Europe,and the South of China.
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