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Natural Gas Geoscience ›› 2020, Vol. 31 ›› Issue (12): 1663-1676.doi: 10.11764/j.issn.1672-1926.2020.06.009

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Accumulation condition and model of buried hill in the Central Uplift， Songliao Basin

Shi-wei YI1(),Ming-peng LI1(),Shu-juan XU1,Xu-jie GUO2,Bao-wen CUI3,Qi-an MENG3,Hong-gang CHENG1,Xue-qiong WU1,Jun-feng CUI1,Li-xian WANG4   

  1. 1.PetroChina Research Institute of Petroleum Exploration & Development，Beijing 100083，China
    2.PetroChina Exploration & Production Company，Beijing 100007，China
    3.Exploration Department of Daqing Oilfield Company，Daqing 163000，China
    4.Exploration Department of Jilin Oilfield Company，Songyuan 138000，China
  • Received:2020-04-29 Revised:2020-06-23 Online:2020-12-10 Published:2020-12-11
  • Contact: Ming-peng LI E-mail:ktb_ysw@petrochina.com.cn;limingpeng@petrochina.com.cn
  • Supported by:
    The China National Science and Technology Major Project(2016ZX05007-003)

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Abstract:

The Central Uplift of Songliao Basin is a large positive buried hill tectonic belt clamped between the east and west rift zones， developed several hydrocarbon-rich sags such as Xujiaweizi， Changling， etc.， located in a favorable area of oil and gas multi-period accumulation， therefore the central uplift has superior conditions for hydrocarbon accumulation. According to contact relation of uplift and rift， combination of migration passage， the hydrocarbon supply style can be divided into six types including fault-fault bilateral consequent type， fault-fault bilateral reverse type， fault-fault one consequent and one reverse type， fault-overlap bilateral consequent type， fault-overlap one consequent and one reverse type and overlap-overlap bilateral consequent type. And the passage system can be divided into five types including fault-network fracture type， glutenite-fault-network fracture type， fault-unconformity-network fracture type， glutenite-unconformity-network fracture type， and glutenite-fault-network fracture-unconformity type. Accumulation and evolution model of the central uplift can be divided into four stages， including fold basement denudated stage， rift-uplift coupled weathering-leaching stage， Central Uplift capping and accumulation stage and Central Uplift stable preservation stage. By analyzing and contrasting accumulation model of the central uplift， the uplift between hydrocarbon-rich sags of fault depression period have the same accumulation condition and have beneficial exploration potential， and are the successive domain in oil and gas exploration， thus buried hill and internal are the main breakthrough target.

Key words: Songliao Basin, Central Uplift, Hydrocarbon supply style, Passage system, Buried hill and internal, Accumulation model

CLC Number: 

  • TE122.1

Fig.1

Tectonic units division and comprehensive stratigraphic column in fault depression period, Songliao Basin"

Fig.2

Reservoir development model of bedrock in Songliao Basin"

Fig.3

Connecting-well section of cap rock from Wells Litan 1, Zhaoshen 3, Longtan 2, Longtan 1 to Wang 902"

Fig.4

Thickness of mudstones from 2nd member to 3rd member of Denglouku Formation in north of the Central Uplift①"

Fig.5

Hydrocarbon supply style of the Central Uplift, Songliao Basin"

Fig.6

Passage system of the Central Uplift, Songliao Basin"

Fig.7

Geochemical characteistics and homogenization temperatures of inclusions in the Central Uplift, Songliao Basin"

Fig.8

Gas reservoir section from Gulong Depression, Central Uplift to Xujiaweizi Depression, Songliao Basin"

Fig.9

Tectonic evolution and accumulation model in the Central Uplift, Songliao Basin"

Fig.10

Burial thermal evolution history of the intersection between line 970 and trace 2 300 in Xuzhong Sag"

Fig.11

Seismic section from Gulong Depression, Central Uplift to Xujiaweizi Depression， Songliao Basin"

Fig.12

Stereo display of the Central Uplift and periphery in Songliao Basin"

Fig.13

Accumulation model of Yingshan West Uplift between Xujiaweizi Depression and Yingshan Depression, Songliao Basin"

Fig.14

Accumulation model of Duiqingshan Uplift between Yingshan Depression and Shuangcheng Depression, Songliao Basin"

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