塔里木盆地顺托果勒低隆起顺北4号走滑断裂带成岩流体类型及活动特征

宋刚; 李海英; 叶宁; 韩俊; 肖重阳; 鲁子野; 李映涛

doi:10.11781/sysydz202204603

塔里木盆地顺托果勒低隆起顺北4号走滑断裂带成岩流体类型及活动特征

doi: 10.11781/sysydz202204603

宋刚^1,,
李海英²,
叶宁^3, ,,
韩俊²,
肖重阳²,
鲁子野³,
李映涛⁴

1.
中国石油化工集团有限公司, 北京 100728
2.
中国石化西北油田分公司勘探开发研究院, 乌鲁木齐 830011
3.
西南石油大学地球科学与技术学院, 成都 610050
4.
中国石化石油勘探开发研究院, 北京 102206

详细信息

作者简介:
宋刚(1978—), 男, 高级工程师, 从事油气领域生产经营管理工作。E-mail: songgang@sinopec.com

通讯作者:
叶宁(1987—), 男, 助理研究员, 从事储层地质及储层地球化学研究。E-mail: yn870104@foxmail.com

中图分类号: TE122.2
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出版历程
- 收稿日期: 2022-03-21
- 修回日期: 2022-06-01
- 刊出日期: 2022-07-28

Types and features of diagenetic fluids in Shunbei No. 4 strike-slip fault zone in Shuntuoguole Low Uplift, Tarim Basin

1.
China Petroleum and Chemical Corporation (SINOPEC), Beijing 100728, China
2.
Research Institute of Exploration and Production, SINOPEC Northwest Oilfield Branch Company, Urumqi, Xinjiang 830011, China
3.
School of Geoscience and Technology, Southwest Petroleum University, Chengdu, Sichuan 610500, China
4.
Petroleum Exploration and Production Research Institute, SINOPEC, Beijing 102206, China

摘要

摘要: 塔里木盆地顺托果勒低隆起顺北4号走滑断裂带是该地区重点勘探目标，中奥陶统碳酸盐岩是主要的含油气层系。断裂活动及伴随断裂活动的断裂流体活动控制了研究区内储层的分布，因此，研究断裂流体的活动特征对勘探工作至关重要。针对研究区顺北4号断裂带内中奥陶统碳酸盐岩裂缝中的方解石进行了岩石学、原位锶同位素、原位稀土元素和U-Pb测年研究。方解石的锶同位素比值为0.708 498~0.709 177，方解石稀土元素表现出明显的Ce负异常、Eu正异常和高Y/Ho比值。方解石U-Pb测年获得的年龄分别为(433±17) Ma和(449±15) Ma。方解石的原位锶同位素和稀土元素特征说明流体充分继承了碳酸盐岩围岩的特征且经历了高温；U-Pb年龄则说明顺北4号断裂带方解石记录的更可能是与阿尔金造山带挤压造山相关的加里东中期Ⅲ幕运动的断裂流体活动。
- 走滑断裂 /
- 成岩流体 /
- 碳酸盐岩 /
- 地球化学 /
- 顺北地区 /
- 塔里木盆地
Abstract: The Shunbei No. 4 strike-slip fault zone is an important exploration target in the Shuntuoguole Low Uplift of Tarim Basin, and the Middle Ordovician carbonate is a major hydrocarbon-bearing stratum. Fault structures and accompanied fluids play a key role for the distribution of carbonate reservoirs, and it is therefore important to study the fluids accompanied with fault evolution. Petrography, in situ Sr isotopic compositions, in situ rare earth elements (REE) and U-Pb dating were carried out to reveal the fluids from which the calcites in fractures precipitated. The calcites in fractures show ⁸⁷Sr/⁸⁶Sr ratios of 0.708 498-0.709 177, and the REE patterns of the calcites are characterized by negative Ce anomaly, positive Eu anomaly and high Y/Ho ratios. The calcite samples show U-Pb isochron age of (433±17) Ma and (449±15) Ma, respectively. The ⁸⁷Sr/⁸⁶Sr ratios and REE patterns of the calcites suggest that parent fluids experienced elevated temperature environment and buffered by carbonate host rocks. The U-Pb isochron age implies that the calcites may record the fault-related fluids during the Ⅲ stage of the Middle Caledonian Movement, which might be associated with the Altyn orogeny.
- strike-slip fault /
- diagenetic fluid /
- carbonates /
- geochemistry /
- Shunbei area /
- Tarim Basin

HTML全文

图 1 塔里木盆地顺北油气田构造位置(a)与地层柱状图(b)

据马永生等^[12]修改。

Figure 1. Tectonic units (a) and stratigraphic column (b) of Shunbei oil & gas field, Tarim Basin

下载: 全尺寸图片幻灯片

图 2 塔里木盆地顺北4号走滑断裂带中—下奥陶统碳酸盐岩储层发育模式示意

Figure 2. Development model of Lower-Middle Ordovician carbonate reservoirs in Shunbei No. 4 strike-slip fault zone, Tarim Basin

下载: 全尺寸图片幻灯片

图 3 塔里木盆地顺北4号走滑断裂带中—下奥陶统碳酸盐岩缝洞充填物特征

a.岩心照片，孔洞中充填巨晶方解石(VC)，另可见近层面发育的裂缝被方解石(C1)充填，其中VC方解石切割缝合线，而缝合线切割C1方解石，顺北A井，7 412.03 m，O₂yj；b，c为a中红框区域的单偏光和阴极光照片，可见C1方解石在阴极射线下具有橙色的发光性；d.岩心照片，缝合线切割两期裂缝，顺北A井，O₂yj；e.岩心照片，高角度裂缝被方解石充填，顺北B井；f，g为d红框中的单偏光和阴极光照片，其中，裂缝中沿边缘向中心依次分布两期方解石(C1、C2)、鞍形白云石(SD)和石英(QZ)；h，i为e红框中的单偏光和阴极光照片，见裂缝被方解石(C2)充填，在阴极射线下具有中等橙色的发光性

Figure 3. Charcteristics of fracture-pore cements in Lower-Middle Ordovician carbonates in Shunbei No. 4 strike-slip fault zone, Tarim Basin

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图 4 塔里木盆地顺北4号走滑断裂带中下奥陶统成岩演化序列示意

Figure 4. Paragenetic sequence of Lower-Middle Ordovician carbonates in Shunbei No.4 strike-slip fault zone, Tarim Basin

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图 5 塔里木盆地顺北地区中下奥陶统裂缝方解石充填物的原位稀土元素配型

PAAS为澳大利亚太古宇后平均页岩成分中的稀土元素。

Figure 5. REEY profiles of fracture cements in Lower-Middle Ordovician carbonates in Shunbei No.4 strike-slip fault zone, Tarim Basin

下载: 全尺寸图片幻灯片

图 6 塔里木盆地顺北4号走滑断裂带中—下奥陶统碳酸盐岩裂缝充填物的U-Pb定年结果

图中绿色数值为协和线的数学理论值。

Figure 6. U-Pb dating of fracture cements in Lower-Middle Ordovician carbonates in Shunbei No.4 strike-slip fault zone, Tarim Basin

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图 7 挤压背景下断裂流体活动示意

Figure 7. Activities of fault-related fluidsin compression environment

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表 1 塔里木盆地顺北4号带方解石C2的原位⁸⁷Sr/⁸⁶Sr比值

Table 1. In situ Sr-isotope analysis of calcite C₂ cement in Shunbei No. 4 strike-slip fault zone, Tarim Basin

样品编号	⁸⁷Sr/⁸⁶Sr	相对误差
SHB4-1-01	0.708 498	0.000 058
SHB4-1-02	0.708 705	0.000 074
SHB4-1-03	0.708 608	0.000 072
SHB4-2-01	0.709 040	0.000 043
SHB4-2-02	0.709 174	0.000 037
SHB4-2-03	0.708 937	0.000 040
SHB4-3-01	0.709 115	0.000 044
SHB4-3-02	0.709 175	0.000 045
SHB4-3-03	0.709 177	0.000 064
SHB4-4-01	0.709 049	0.000 074
SHB4-4-02	0.709 051	0.000 069
SHB4-4-03	0.709 145	0.000 059
SHB4-4-04	0.709 083	0.000 075
SHB4-6-01	0.709 127	0.000 072
SHB4-6-02	0.708 847	0.000 178
SHB4-6-03	0.709 111	0.000 097

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表 2 塔里木盆地顺北4号段裂带方解石C2的原位微量元素含量

Table 2. In situ trace element contents of calcite C₂ cement in Shunbei No. 4 strike-slip fault zone, Tarim Basin

微量元素	样品
微量元素	SHB4-2-1	SHB4-2-2	SHB4-3-1	SHB4-3-2	SHB4-3-3	SHB4-4-5	SHB4-4-3	SHB4-4-8	SHB4-4-9	SHB4-4-10	SHB4-4	SHB4-5
Al/10^-6			0.167	0.003	0.086	0.172		9.576	0.031	0.175	0.090	0.100
Sc/10^-6	0.017	0.049	0.070	0.119	0.098	0.061	0.062	0.051	0.077	0.057	0.550	0.490
Mn/10^-6	79.0	73.5	73.8	118.1	108.4	69.3	125.2	59.0	106.6	117.4	210.7	213.0
Sr/10^-6	301.1	497.8	599.3	421.6	184.7	381.4	105.4	543.8	511.8	223.9	174.0	181.0
Ba/10^-6	0.058	0.340	0.341	0.262	0.063	0.165		0.037	0.265	0.025	0.059	0.190
La/10^-6	0.007	0.012	0.006	0.022	0.005	0.007	0.072	0.206	0.675	1.113	2.460	1.670
Ce/10^-6	0.013	0.024	0.008	0.030	0.010	0.028	0.161	0.272	1.368	2.703	6.240	4.240
Pr/10^-6	0.002	0.005	0.001	0.005	0.003	0.006	0.026	0.045	0.251	0.529	0.773	0.512
Nd/10^-6	0.012	0.015	0.006	0.021	0.014	0.018	0.123	0.204	1.080	2.437	2.890	1.900
Sm/10^-6	0.001	0.008	0.003	0.005	0.003	0.006	0.030	0.041	0.273	0.706	0.640	0.410
Eu/10^-6	0.001	0.003	0.002	0.008	0.002	0.003	0.013	0.011	0.169	0.245	0.163	0.105
Gd/10^-6	0.003	0.008	0.002	0.006	0.005	0.008	0.037	0.051	0.362	0.995	0.624	0.385
Tb/10^-6	0.000	0.001	0.000	0.001	0.001	0.002	0.004	0.006	0.052	0.169	0.081	0.054
Dy/10^-6	0.002	0.004	0.003	0.006	0.006	0.008	0.023	0.028	0.326	1.137	0.448	0.318
Y/10^-6	0.028	0.081	0.035	0.056	0.067	0.096	0.213	0.281	2.637	8.742	2.570	2.070
Ho/10^-6	0.000	0.002	0.000	0.001	0.002	0.002	0.004	0.005	0.062	0.237	0.086	0.061
Er/10^-6	0.001	0.004	0.001	0.002	0.003	0.005	0.013	0.010	0.153	0.627	0.218	0.154
Tm/10^-6	0.000	0.000	0.000	0.000	0.000	0.000	0.001	0.001	0.015	0.073	0.031	0.019
Yb/10^-6	0.001	0.001	0.001	0.001	0.002	0.003	0.007	0.003	0.079	0.388	0.166	0.135
Lu/10^-6	0.000	0.000	0.000	0.000	0.000	0.000	0.001	0.000	0.008	0.049	0.023	0.020
∑REE/10^-6	0.05	0.09	0.04	0.11	0.06	0.10	0.52	0.89	4.87	11.41	14.84	9.98
Eu异常	4.18	2.35	4.52	8.39	1.86	1.96	2.28	1.40	2.84	1.44	1.35	1.34
Ce异常	0.72	0.71	0.64	0.67	0.58	0.85	0.83	0.65	0.75	0.76	1.03	1.05
Y/Ho	67.6	52.8	87.2	57.9	44.2	39.2	53.2	54.9	42.3	37.0	30.0	33.9

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