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Diagenetic and paleogeothermal evolution of the clay minerals in the Center Uplift Belt and its adjacent region of Huimin Sag,Jiyang Depression

Ni Jin-long1,2,3,4,Zhang Hong3,Tang Xiao-ling5,Han Shuai3   

  1. 1.Key Laboratory of Gold Mineralization Processes and Resource Utilization Subordinated to the Ministry of Land and
    Resources,Ji’nan 250013,China;2.Key Laboratory of Metallogenic Geological Process and Resources Utilization in
    Shandong Province,Ji’nan 250013,China;3.Shandong Provincial Key Laboratory of Depositional Mineralization &
    Sedimentary Minerals,Shandong University of Science and Technology,Qingdao 266590,China;4.Laboratory for Marine
    Mineral Resources,Qingdao National Laboratory for Marine Science and Technology,Qingdao 266071,China;5.College
    of Chemistry & Environmental Engineering,Shandong University of Science and Technology,Qingdao 266590,China
  • Received:2015-12-08 Revised:2016-02-15 Online:2016-10-10 Published:2016-10-10

Abstract: Huimin sag,located in Shengli Oilfield of Shandong province,is one of the most important enrichment zones of oil and gas.It is favorable to further understand the geologic process about this tectonic belt by study of the diagenetic and paleogeothermal evolution of the clay minerals.Abundant samples were picked from the Central Uplift and Linnan sub-sag,and we carried out the analysis of clay mineral component and paleogeotherm by X-ray and electronic probe experiment.The results are as follows:(1)The clay minerals in the central uplift and Linnan sub-sag of Huimin Depression of Shahejie Formation(Es)are composed of kaolinite(K),illite/smectite mixed-layer mineral(I/S),illite(I)and chlorite(Chl).As the whole,the mineral composition indicates that it is at low thermal evolution stage of the clay minerals and the tectonic zones.(2)The diagenesis is generally middle diagenetic stage,and two sub-stage were divided,namely,the early stage,the content of illite in the I/S between 38.2% and 60.3%;and the late stage,the content of illite in the I/S between 60.3% and 82.4%.The change depth boundary of the two sub-stages is different,such as,1 700 meter in the Central Uplift Belt,and 2 600 meter in Linnan Sub-sag.(3)The thermal evolution level is lower in the Central Uplift Belt than that in the Linnan Sub-sag,which indicated the Central Uplift Belt possibly rapidly uplifted from the depositional stage of Es2,and resulted in the different diagenesis background from the Linnan Sub-sag;The Paleogeotherm gradient in Linnan Sub-sag is 40.8℃/km,but the obviously abnormal calculated result was obtained in the center uplift belt,e.g.76.72℃/km,which indicates the strong uplift and erosion(the denuded thickness is 880m)in the central uplift belt.

Key words: Huimin Sag, Uplift center belt, Shahejie Formation, Clay mineral, Paleogeotherm

CLC Number: 

  • TE121.1
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