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《Acta Geologica Sinica》 2015-05
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Thermal Evolution History of Yanchang Formation in the Southeastern Margin of the Ordos Basin:Evidence from Vitrinite-Reflectance and Apatite Fission-Track

HUANG Zhigang;REN Zhangli;CHEN Yulin;Department of Earth Science,Taiyuan University of Technology;Department of Geology,Northwest University;Oil Gas Evaluation Centre of CPL;  
Six samples collected from the Late Triassic Yanchang Formation in the southeastern margin of Ordos Basin and the other six sandstone samples collected also from the same formation were employed to obtain Vitrinite reflectance(Ro)data and apatite fission track(AFT)dating,respectively.The Rodata and AFT results show that the thermal evolution of organic in the southeastern margin of Ordos Basin is higher than that in other places,with Roranging from 0.65% to 0.78%in the Hancheng area.Due to the effect of Mesozoic intracontinental orogensis in Qinling,the Roof Triassic Yanchang Formation reaches 2.67%~3.71%.The AFT data shows that the value of the AFT central age decreased with the strata growing older.Our results show that the southeastern margin of the Ordos Basin experienced an important structure-heat event at late Mesozoic(100 Ma).Hancheng area had a different thermal evolution history from the Luonan area,with the Hancheng area belonging to buried heating type and the Luonanjingcun section to the type controlled by tectonic-magmatic activities.This understanding is consistent with from field geological evidence.
【Fund】: 国家自然科学基金项目(编号41372128);; 西北大学大陆动力学国家重点实验室(编号BJ08133-1);; 国家重大专项(编号2011ZX05005-004-007HZ)资助成果
【CateGory Index】: P618.13
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