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Petrological evidence of kaolinite transformation to dawsonite |
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| Authors: | GUI Lily LIU Li YU Miao LIU Na YANG Huidong ZHANG Yongmei |
| Institution: | 1. College of Earth Sciences, Jilin University, Changchun 1300061, China;CNPC Key Laboratory for Basin Structure and Hydrocarbon Accumulation, Research Institute of Petroleum Exploration and Development, PetroChina , Beijing 10083, China 2. College of Earth Sciences, Jilin University, Changchun 1300061, China 3. College of Earth Sciences, Jilin University, Changchun 1300061, China;Exploration and Development Research Institute, Jilin Oilfield Branch, PetroChina, Songyuan 138001, Jilin, China 4. Exploration and Development Research Center, Qinghai Oilfield, CNPC, Dumhuang 736202, Gansu, China |
| Abstract: | Clay minerals,especially authigene kaolinite,are abundant in the dawsonite-bearing sandstone from the Gudian and Qian’an regions in the southern Songliao Basin. The relationship between dawsonite and kaolinite has been investigated based on drilling data from 50 wells in the Jilin Oil Field and petrological characteristics analyses on 23 core samples from the Gudian and Qian’an regions. The study revealed a negative relationship between the content of dawsonite and kaolinite,suggesting that kaolinite was replaced by the dawsonite. Combined with thermodynamics and geochemical analysis published previously,it is concluded that kaolinite is unstable under CO2-rich environments and can transform into dawsonite. |
| Keywords: | kaolinite dawsonite transformation Songliao Basin |
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