Oil & Gas Geology ›› 2006, Vol. 27 ›› Issue (4): 549-556.doi: 10.11743/ogg20060417

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Petrology and genesis of Mesozoic volcanic rocks in Tuo32 well block of Liaohe oilfield

Zhao Hailin1,2, Li Xiaoguang3, Chen Zhenyan3, Di Yongjun2, Liu Jie3, Hong Shuxin4, Zhao Guanghui2   

  1. 1. State Key Labrotary of Geological Process and Mineral Resources · Key Labrotary of Lithospheric Tectonics and Exploration, Ministry of Education, China University of Geosciences, Beijing 100083;
    2. China University of Geosciences, Beijing 100083;
    3. Exploration and Development Research Institute, Liaohe Oilfield Company, PetroChina, Panjin, Liaoning 124010;
    4. Exploration and Development Research Institute, Daqing Co.ltd, PetroChina, Daqing, Heilongjiang 163712
  • Received:2006-02-20 Online:2006-08-25 Published:2012-01-16

Abstract:

The types of volcanic rocks in Tuo32 well block of Liaohe oilfiled include rhyolite,trachyandesite,andesite,rhyolitic breccia,rhyolitic eruptive tuff,andestic breccia,and andestic eruptive tuff.The volcano erupted five times in two phases in about(97.37?1.41)Ma and(79.52?1.25)Ma,with the first phase in the late Early Cretaceous and the second phase in the middle Late Cretaceous. The 'reverse' phenomenon in volcanic eruptions is explained as the result of a zonal lava chamber based on the theory of lava hydrokinetics.Models of the zonal lava chamber and the surface distribution of the volcanic rocks are built.

Key words: volcanic rocks and their types, eruptive time, beltshaped lava chamber, Mesozoic volcanic rocks, Niuxintuo area, Liaohe oilfield

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