塔里木盆地顺北地区克拉通内走滑断裂带中-下奥陶统储集体方解石脉形成及其与油气充注耦合关系

doi:10.11743/ogg20230110

Abstract

Abstract:

Shunbei oil/gas field is of the ultra-deep carbonate type controlled by multi-stage strike-slip faulting within the craton. The significant differences on the oil/gas property and abundance are shown in different fault zones even different segments in a fault zone. An integration of the core and thin section observation， cathodoluminescence， in-situ trace and rare earth element （REE） analysis， systematic analysis of fluid inclusions， is applied to study the sequence of fracture vein formation， sources of vein-forming fluids and their coupling relationships with hydrocarbon charging in the Middle-Lower Ordovician reservoir of the No.1 and 5 strike-slip fault zones in Shunbei area. We also investigate the factors controlling differential hydrocarbon accumulation in Shunbei area while understanding the evolution of strike-slip faults and the hydrocarbon accumulation pattern. The results show that there are at least four phases of calcite vein development， that is， Cal-1， Cal-2， Cal-3， and Cal-4， respectively， in the Middle-Lower Ordovician reservoir of the No. 1 and 5 strike-slip fault zones in Shunbei area. The vein-forming fluids of Cal-1 are mainly sea-sourced fluids， while that of Cal-2， Cal-3 and Cal-4 are derived from diagenetic fluids in the reservoir where the veins occur. The formation of Cal-2， Cal-3 and Cal-4 calcite veins is associated with tectonic activities and hydrocarbon charging in the Late Caledonian to Early Hercynian， the Late Hercynian to Indosinian， and the Yanshan-Himalayan， respectively. The strike-slip fault zones are different in hydrocarbon charging， as shown by that the main charging phase of the No. 5 fault zone was during the Late Hercynian to Indosinian， while the main charging period of No. 1 fault zone was during the Late Hercynian to Indosinian， and Yanshan-Himalayan. The differential hydrocarbon charging controlled by strike-slip fault structural style and evolution history is the key to differential hydrocarbon accumulation in Shunbei area.

Key words: calcite vein, strike-slip fault zone, differential hydrocarbon accumulation, hydrocarbon charging, ultra-deep stratum, carbonate oil/gas field, Shunbei area, Tarim Basin

CLC Number:

TE122.3

Jianzhang LIU, Zhongxian CAI, Changyu TENG, Heng ZHANG, Chen CHEN. Coupling relationship between formation of calcite veins and hydrocarbon charging in Middle-Lower Ordovician reservoirs in strike-slip fault zones within craton in Shunbei area， Tarim Basin[J]. Oil & Gas Geology, 2023, 44(1): 125-137.

Figures/Tables 8

Fig.1

Fig.2

Fig.3

Table 1

Contents and ratios of REEs and some trace elements in calcite veins and host-rocks of the No. 1 and 5 fault zones in Shunbei area"

断裂带	方解石脉/围岩（样品数量）	Mn含量/ （μg·g^-1）	Fe含量/ （μg·g^-1）	Fe /Mn	U/Th	?REE/ （μg·g^-1）	?LREE/?HREE
顺北1号	Cal-2（N=4）	$130.7 ? ~ ? 136.4 133.2$	$441.0 ? ~ ? 1024.5 625.1$	$3.4 ? ~ ? 7.5 4.7$	$1.1 ? ~ ? 1.4 1.2$	$2.2 ? ~ ? 4.8 3.7$	$1.8 ? ~ ? 3.8 3.1$
	Cal-3（N=4）	$25.1 ? ~ ? 30.3 28.0$	$90.8 ? ~ ? 272.6 174.5$	$3.0 ? ~ ? 9.2 6.2$	$1.4 ? ~ ? 100.0 28.2$	$10.1 ? ~ ? 18.3 14.7$	$6.7 ? ~ ? 13.7 9.4$
	Cal-4（N=2）	$31.9 ? ~ ? 47.4 39.6$	$1 ? 498.4 ? ~ ? 2 ? 264.6 1 ? 881.5$	$31.6 ? ~ ? 71.1 51.3$	$4.1 ? ~ ? 7.2 5.7$	$6.6 ? ~ ? 9.7 8.2$	$8.9 ? ~ ? 76.4 42.6$
	灰岩（N=3）	$18.3 ? ~ ? 27.0 22.2$	$158.3 ? ~ ? 199.4 183.7$	$5.9 ? ~ ? 10.9 8.6$	$1.5 ? ~ ? 3.1 2.2$	$18.5 ? ~ ? 28.9 23.7$	$6.1 ? ~ ? 11.9 9.0$
顺北5号	Cal-1（N=3）	$3.3 ? ~ ? 8.9 5.4$	$92.4 ? ~ ? 97.0 94.0$	$10.9 ? ~ ? 27.9 20.5$	$1.0 ? ~ ? 48.3 24.7$	$0.02 ? ~ ? 0.3 0.2$	$0.9 ? ~ ? 4.2 2.7$
	Cal-2（N=5）	$38.9 ? ~ ? 92.0 65.2$	$161.3 ? ~ ? 698.8 407.9$	$4.1 ? ~ ? 7.6 6.0$	$2.4 ? ~ ? 3.2 2.8$	$1.8 ? ~ ? 7.3 4.4$	$3.9 ? ~ ? 4.6 4.4$
	Cal-3（N=5）	$36.6 ? ~ ? 110.5 70.9$	$77.8 ? ~ ? 236.8 130.9$	$1.2 ? ~ ? 2.1 1.8$	$0.9 ? ~ ? 149.1 50.3$	$15.8 ? ~ ? 21.3 17.7$	$6.1 ? ~ ? 19.7 11.4$
	Cal-4（N=2）	$156.6 ? ~ ? 212.2 184.4$	$1 ? 248.9 ? ~ ? 1 ? 845.9 1 ? 547.4$	$8.0 ? ~ ? 8.7 8.4$	$2.2 2.2$	$1.8 ? ~ ? 4.2 3.0$	$4.5 ? ~ ? 6.8 5.7$
	灰岩（N=3）	$27.1 ? ~ ? 139.1 65.5$	$331.7 ? ~ ? 745.1 604.8$	$5.4 ? ~ ? 27.3 14.5$	$0.5 ? ~ ? 0.9 0.8$	$8.3 ? ~ ? 20.3 12.6$	$5.1 ? ~ ? 6.1 5.5$

Table 1

Fig.4

Fig.5

Fig.6

Fig.7

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Coupling relationship between formation of calcite veins and hydrocarbon charging in Middle-Lower Ordovician reservoirs in strike-slip fault zones within craton in Shunbei area， Tarim Basin

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