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Natural Gas Geoscience ›› 2020, Vol. 31 ›› Issue (7): 993-1003.doi: 10.11764/j.issn.1672-1926.2020.02.008

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Influence of tectonic evolution of foreland basin in northwestern Sichuan Basin on Paleozoic marine hydrocarbon accumulation

Bin LI1,2(),Wen-hua MEI1,2,Qi-qi LI1,3,Qin-gong ZHUO4,Xue-song LU4,Qiang GUO1   

  1. 1.School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, China
    2.State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu 610500, China
    3.China University of Geosciences, Wuhan 430074, China
    4.PetroChina Research Institute of Petroleum Exploration and Development, Beijing 100083, China
  • Received:2019-12-10 Revised:2020-02-27 Online:2020-07-10 Published:2020-07-02
  • Supported by:
    State Key Laboratory of Shale Oil and Gas Enrichment Mechanisms and Effective Development Project(GSYKY-B09-33)

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Abstract:

Aim to the complexity and zonality of Paleozoic marine hydrocarbon accumulation caused by foreland basin tectonic in northwestern Sichuan Basin, the influence and differential characteristics of foreland basin tectonic evolution on Paleozoic marine hydrocarbon accumulation are analyzed from the perspective of reservoir forming conditions. It is supposed that the foreland basin structure in western Sichuan Basin longitudinally promoted the thermal evolution of the Paleozoic source rocks into the high-mature and over-mature stage. Laterally, there was a delay effect on the source rocks in the thrust belt and depression zone. The reservoir with characteristics of low porosity and permeability was caused by foreland basin squeezing action, and the porosity of the reservoir conforms to the compaction law. And the uplift destroyed the capping ability of the cover in the foreland thrust belt, reduced the effectiveness of traps, and fault block traps and tectonic-lithologic traps are developed in an area covering the front of thrust belt, and the preserve condition are well. The Paleozoic oil and gas accumulation in the study area has obvious zonation, in which the foreland thrust nappe belt affected by lateral migration system has the characteristics of late adjustment of early oil to gas, and reservoir controlled by preservation. The area in front of thrust belt is affected by stage migration system of permeable bed-fault, with characteristics of multi-source injection, multi-period migration and accumulation, and reservoir controlled by source faults. The depression zone is characterized by near source injection, continuous hydrocarbon supply, and reservoir controlled by vertical migration system of intraformational faults. The comprehensive analysis shows that the area in front of thrust belt is a favorable hydrocarbon accumulation area of Paleozoic marine formation.

Key words: Northwestern Sichuan Basin, Structure evolution of foreland basin, Paleozoic, Marine oil and gas, Accumulation model

CLC Number: 

  • TE122.1

Fig.1

Wells location of Paleozoic in northwestern Sichuan Basin"

Fig.2

Profile of seismic line 2010SH03 in northwestern Sichuan Basin （section location is shown in Fig.1)①"

Table 1

Statistics of source rock in the Paleozoic of northwest Sichuan Basin"

层

位

主要岩性厚度/mTOC/%RO/%（沥青等效反射率）有机质类型取样点
范围

平均值

（样品数）

范围

平均值

（样品数）

范围

平均值

（样品数）

P3d灰黑色硅质泥岩10~5537（8）0.18~8.102.08（8）1.49~2.121.75（6）Ⅱ1—Ⅱ2矿1井、河2井、长江沟、吴家1井、大两会、扁1井等
P3l（P3w）生物灰岩、生屑灰岩、煤0~9054（12）0.25~6.721.92（9）1.52~2.171.73（10）Ⅱ1—Ⅱ2、Ⅲ矿1井、矿3井、金真村、老荒坡、剑丰、乌木沱、大两会、桥亭、朝天等
P2m生屑泥晶灰岩25~250138（12）0.07~2.580.85（21）1.10~3.372.00（22）Ⅰ—Ⅱ1通口、葛上岩、青杠坡、吴家1井、射1井、扁1井、矿3井等
P2q生屑泥晶灰岩30~7556（9）0.06~4.820.79（11）1.50~2.321.79（4）Ⅰ—Ⅱ1通口、双探3、龙17井、矿3井等
S1l黑色页岩、深灰色泥岩0~20050（3）0.09~2.330.91（5）1.49~2.371.82（3）Ⅰ—Ⅱ1南江桥亭、南江杨坝、川北等
∈1q黑色泥岩20~300163（7）0.60~6.202.81（9）1.40~3.322.13（7）Ⅰ朝天、火石岭、田坝等

Fig.3

Simulation diagram of single well thermal evolution in northwest well Sichuan Basin"

Fig.4

Hydrocarbon generation history of the main Paleozoic source rock in northwestern Sichuan Basin"

Table 2

Statistical table of basic reservoir characteristics of Qixia Formation in northwestern Sichuan Basin①"

构造带样本个数孔隙度/%渗透率/(10-3 μm2)储层岩石类型储集空间类型样本点

逆冲

推覆带

N=2540.13~16.512.260.0~7840.608粉细晶云岩，豹斑云质灰岩晶间孔，裂缝和溶洞矿2井，矿1井，天井山

前缘

隐伏带

N=2470.23~7.591.8250.0~94.25.14粉细晶针孔云岩裂缝—孔隙型双探3井
坳陷带N=1030.1~0.920.490.0~17.71.73泥—亮晶灰岩孔隙型龙17井，元坝3，吴家1井，龙4井

Fig.5

Histogram porosity and permeability of Dolomite Reservoir in Qixia Formation, Northwest Sichuan"

Table 3

Statistics of Paleozoic preservation condition in northwestern Sichuan Basin"

构造带盖层厚度地层水矿化度地层压力代表井
逆冲推覆带①龙潭组泥页岩厚度：36.1 m;②中下三叠统膏岩厚度：86.6 m① 茅口组，硫酸钠型，矿化度：23.558 g/L；②栖霞组，氯化钙型，矿化度：45.4 g/L；③志留系—奥陶系矿化度:32.325 g/L，水型：CaCl2①栖霞组地层压力系数0.86；②石炭系压力系数0.79矿3
前缘隐伏带①龙潭组泥页岩厚度：96 m;②中下三叠统膏岩厚度：310 m①茅口组水型：CaCl2,地层压力：82MPa；②栖霞组，氯化钙型，地层压力：73.5MPa。①茅口组压力系数：1.2；②栖霞组地层压力系数：1.02

双探1,

双探3

坳陷带①龙潭组泥页岩厚度：37 m;②中下三叠统膏岩厚度：270 m茅口组，重碳酸钠型，矿化度16.89 g/L地层压力系数1.36关基井，扁1，吴家1

Fig.6

Accumulation model of Paleozoic gas reservoir in northwestern Sichuan Basin"

Fig.7

Carbon Isotope correlation of kerogen and ethane of Paleozoic source rocks in northwestern Sichuan Basin(data of Hewanchang, Wujiaba and Kuangshanliang according to HUANG et al.[5],2011; other data according to LIU et al.[28],2016)."

Fig.8

Schematic map of accumulation conditions of Paleozoic reservoirs in northwestern Sichuan Basin"

Fig.9

Schematic map of Paleozoic reservoir in northwestern Sichuan Basin （BB’ section location is shown in Fig.1）"

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