塔里木盆地富满油田走滑断裂演化特征及其对油气运聚的影响

doi:10.12108/yxyqc.20260204

Lithologic Reservoirs ›› 2026, Vol. 38 ›› Issue (2): 44-55.doi: 10.12108/yxyqc.20260204

• PETROLEUM EXPLORATION • Previous Articles Next Articles

Tectonic evolution of strike-slip faults and its impact on hydrocarbon migration and accumulation in Fuman Oilfield， Tarim Basin

CHANG Shaoying¹^,²(), DONG Keliang¹^,³(), ZENG Jianhui¹^,³, YANG Jining¹^,³, WANG Mengxiu², LIU Lingli²

¹ State Key Laboratory of Petroleum Resources and Engineering， China University of Petroleum （Beijing）， Beijing 102249， China
² Hangzhou Research Institute of Geology， PetroChina， Hangzhou 310023， China
³ College of Geosciences， China University of Petroleum （Beijing）， Beijing 102249， China

Received:2025-02-28 Revised:2025-04-16 Online:2026-03-01 Published:2026-02-10

Abstract

Abstract:

Multi-stage activities of strike-slip faults of Fuman Oilfield in Tarim Basin significantly control hydrocarbon migration and accumulation in deep to ultra-deep reservoirs. Based on 3D seismic data interpretation of Fuman Oilfield， structural characteristics and tectonic evolution of F_I5 fault， F_I7 fault， F_I16 fault， and F_I17 fault were delineated， and their influences on hydrocarbon migration and accumulation were analyzed. The results show that：（1） F_I5 fault， F_I7 fault， F_I16 fault， and F_I17 fault primarily underwent four stages of tectonic evolution： Early Caledonian， episode Ⅰ of middle Caledonian， episode Ⅲ of middle Caledonian， and late Caledonian-early Hercynian. Among them， episode Ⅰ of middle Caledonian and episode Ⅲ of middle Caledonian were the main active periods. F_I5 fault and F_I17 fault were more active than F_I7 fault and F_I16 fault, with F_I16 fault exhibi-ting the weakest activity. （2） F_I5 fault and F_I17 fault have source connectivity and improve the reservoir property. F_I7 fault has no source connectivity， but its conductivity and reservoir improvement ability are good， while F_I16 fault has poor source connectivity， conductivity, and reservoir improvement ability. （3） During late Caledonian， oil and gas underwent certain scale vertical charging along F_I5 fault and F_I17 fault， while migration and enrichment rarely occurred along F_I7 fault， and the scale of vertical charging along F_I16 fault zone was relatively small. In late Hercynian， large-scale vertical hydrocarbon migration and accumulation occurred along F_I5 fault and F_I17 fault. F_I7 fault did not connect to hydrocarbon source， resulting in limited vertical migration and accumulation of oil and gas along it. Lateral migration and accumulation may have occurred and had a certain scale， while the scale of vertical migration and accumulation along F_I16 fault was relatively small. （4） During Himalayan， Lower Cambrian source rocks in the eastern part of Fuman area entered the over-mature gas generation stage. While Middle Cambrian gypsum-salt layers failed to form an effective seal， leading to significant gas washing in petroleum reservoirs near F_I16 fault and F_I17 fault， resulting in an overall increase in gas-oil ratio.

Key words: strike-slip fault, tectonic evolution, source connectivity, hydrocarbon migration and accumulation, Caledonian movement, Lower Paleozoic, Fuman Oilfield, Tarim Basin

CLC Number:

TE122.1

CHANG Shaoying, DONG Keliang, ZENG Jianhui, YANG Jining, WANG Mengxiu, LIU Lingli. Tectonic evolution of strike-slip faults and its impact on hydrocarbon migration and accumulation in Fuman Oilfield， Tarim Basin[J].Lithologic Reservoirs, 2026, 38(2): 44-55.

Figures/Tables 11

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TRENDMD:

断裂	井名	错断距离/m	变形强度
F_I5	跃满20-1 X	38.79	0.09
	果勒301 H	33.93	0.10
	果勒3-H12	41.78	0.06
F_I7	跃满2-5 X	—	—
	跃满5-1	—	—
	跃满601	—	—
F_I16	玉科301-H1	17.55	0.08
	玉科3	23.40	0.04
	玉科3-H2	16.01	0.03
F_I17	满深1-H2	60.51	0.40
	满深1	47.01	0.73
	满深4	49.98	0.18

断裂	井名	厚度/m	错断距离/m	变形强度
F_I5	跃满20-1 X	492.49	36.90	0.05
	果勒3-H12	468.22	60.67	0.11
	果勒3	460.69	57.50	0.08
F_I7	跃满2-5 X	465.21	26.23	0.09
	跃满5-1	451.24	48.16	0.18
	跃满601	486.72	17.54	0.02
F_I16	玉科301-H1	417.77	23.88	0.05
	玉科3	435.26	19.79	0.04
	玉科3-H2	418.36	12.56	0.03
F_I17	满深502 H	1 017.53	51.77	0.31
	满深3	1 014.78	49.85	0.18
	满深1	982.20	162.98	0.75

断裂	井名	漏失量/m³	储集系数
F_I5	跃满20-H3	1 482.40	1.23
	跃满20 C	505.40	0.42
	果勒3-H3	1 487.82	1.23
	果勒3-H12	1 057.45	0.88
F_I7	跃满2-5 X	1 587.60	1.32
	跃满10	845.61	0.70
	跃满5-4 X	749.15	0.62
	跃满601	215.10	0.18
F_I16	玉科301-H5	625.90	0.52
	玉科301	552.32	0.46
	玉科3	967.29	0.80
	玉科3-H2	431.88	0.36
F_I17	满深502 H	1 761.45	1.42
	满深3	2 463.00	2.04
	满深1-H2	1 360.84	1.13
	满深4	470.00	0.39

Tectonic evolution of strike-slip faults and its impact on hydrocarbon migration and accumulation in Fuman Oilfield， Tarim Basin

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