Carbon isotope composition and correlation across the Cambrian-Ordovician boundary in Kalpin Region of the Tarim Basin, China  被引量:10

Carbon isotope composition and correlation across the Cambrian-Ordovician boundary in Kalpin Region of the Tarim Basin, China

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作  者:JING XiuChun DENG ShengHui ZHAO ZongJu LU YuanZheng ZHANG ShiBen 

机构地区:[1]School of the Earth Sciences and Resources,China University of Geosciences,Beijing 100083,China [2]Research Institute of Petroleum Exploration and Development,Beijing 100083,China

出  处:《Science China Earth Sciences》2008年第9期1317-1329,共13页中国科学(地球科学英文版)

基  金:the Tarim Oilfield Company, PetroChina, the Innovating Foundation of Research Institute of Petroleum Exploration & Development, PetroChina and the Outstanding Doctoral Dissertation Support Foundation of China University of Geo-sciences (Beijing)

摘  要:Biostratigraphically constrained sequences at the Wushi Yingshan and Kalpin Cement Plant sections (Kalpin Region; Tarim Basin) were densely sampled for geochemical studies. Carbonates across the Cambrian-Ordovician boundary of both sections mainly record negative carbon isotope values. Stable isotope curves show four negative and four positive excursions appearing alternately at the Wushi Yingshan section and five negative alternating with five positive excursions at the Kalpin Cement Plant section. The carbon isotope logs of these two sections are correlated with the international Cambrian-Ordovician boundary key sections: (1) Dayangcha section in China, (2) Green Point section in Canada, (3) Black mountain section in Australia and (4) Lowson Cove section in USA. These correlations suggest that the Cambrian-Ordovician boundary of the Wushi Yingshan section and the Kalpin Cement Plant section can be placed within a particular horizon that also corresponds to the observed biostratigraphic units.Biostratigraphically constrained sequences at the Wushi Yingshan and Kalpin Cement Plant sections (Kalpin Region; Tarim Basin) were densely sampled for geochemical studies. Carbonates across the Cambrian-Ordovician boundary of both sections mainly record negative carbon isotope values. Stable isotope curves show four negative and four positive excursions appearing alternately at the Wushi Yingshan section and five negative alternating with five positive excursions at the Kalpin Cement Plant section. The carbon isotope logs of these two sections are correlated with the international Cambrian-Ordovician boundary key sections: (1) Dayangcha section in China, (2) Green Point section in Canada, (3) Black mountain section in Australia and (4) Lowson Cove section in USA. These correlations suggest that the Cambrian-Ordovician boundary of the Wushi Yingshan section and the Kalpin Cement Plant section can be placed within a particular horizon that also corresponds to the observed biostratigraphic units.

关 键 词:CAMBRIAN-ORDOVICIAN BOUNDARY carbon ISOTOPES CONODONTS TARIM Basin 

分 类 号:P597[天文地球—地球化学]

 

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