鄂尔多斯盆地杭锦旗地区二叠系地层水地球化学特征和来源

赵永强; 倪春华; 吴小奇; 朱建辉; 刘光祥; 王付斌; 贾会冲; 张威; 齐荣; 安川

doi:10.11781/sysydz202202279

鄂尔多斯盆地杭锦旗地区二叠系地层水地球化学特征和来源

doi: 10.11781/sysydz202202279

赵永强^{1, 2,},
倪春华^{1, 2},
吴小奇^{1, 2},
朱建辉^{1, 2},
刘光祥³,
王付斌⁴,
贾会冲⁵,
张威⁵,
齐荣⁵,
安川⁵

1.
中国石化石油勘探开发研究院无锡石油地质研究所, 江苏无锡 214126
2.
中国石化油气成藏重点实验室, 江苏无锡 214126
3.
中国石化石油勘探开发研究院, 北京 102206
4.
中国石化华北油气分公司油气勘探管理部, 郑州 450006
5.
中国石化华北油气分公司勘探开发研究院, 郑州 450006

基金项目:

国家自然科学基金项目 42172149

国家自然科学基金项目 41872122

国家科技重大专项 2016ZX05002-006

详细信息

作者简介:
赵永强(1973—)，男，博士，高级工程师，从事油气成藏研究。E-mail: zhaoyq.syky@sinopec.com

中图分类号: TE133
计量
- 文章访问数: 405
- HTML全文浏览量: 84
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- 被引次数: 0
出版历程
- 收稿日期: 2021-07-05
- 修回日期: 2022-02-20
- 刊出日期: 2022-03-28

Geochemical characteristics and source of Permian formation water in Hangjinqi area, Ordos Basin

ZHAO Yongqiang^{1, 2
,},
NI Chunhua^{1, 2},
WU Xiaoqi^{1, 2},
ZHU Jianhui^{1, 2},
LIU Guangxiang³,
WANG Fubin⁴,
JIA Huichong⁵,
ZHANG Wei⁵,
QI Rong⁵,
AN Chuan⁵

1.
Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214126, China
2.
SINOPEC Key Laboratory of Hydrocarbon Accumulation, Wuxi, Jiangsu 214126, China
3.
Petroleum Exploration and Production Research Institute, SINOPEC, Beijing 102206, China
4.
Department of Oil and Gas Exploration Management, SINOPEC North China Branch, Zhengzhou, Henan 450006, China
5.
Research Institute of Exploration and Development, SINOPEC North China Branch, Zhengzhou, Henan 450006, China

摘要

摘要: 杭锦旗地区二叠系是近年来鄂尔多斯盆地重要的天然气增储上产领域之一，其气水关系复杂，目前对该区地层水成因和来源的研究较为薄弱。通过对杭锦旗地区二叠系地层水样品开展常量组分、微量元素和氢、氧同位素分析，揭示地球化学特征对地层水来源的指示意义。杭锦旗地区二叠系地层水主体为CaCl₂型，泊尔江海子断裂以北和以南地区地层水矿化度平均分别为52.1 g/L和41.9 g/L；不同类型水化学特征参数均指示了地层封闭性较好，地层水在埋藏过程中经历了较强的浓缩变质作用，天然气保存条件较好；地层水主体为蒸发浓缩后的陆相地层水，地层中发生了斜长石的钠长石化作用和胶结物的白云岩化作用；地层水氢、氧同位素值主体分别介于-81‰~-75‰和-12.1‰~-8.8‰，水岩相互作用整体明显弱于苏里格气田。受晚白垩世以来区域性抬升过程中凝析水混入、地表水沿断裂渗入等因素影响，少数地层水样品具有偏低的氢同位素值。
- 矿化度 /
- 微量元素 /
- 氢氧同位素 /
- 地层水 /
- 二叠系 /
- 杭锦旗地区 /
- 鄂尔多斯盆地
Abstract: The Permian stratum in Hangjinqi area is one of the important fields to increase gas reserves and outputs in the Ordos Basin in recent years. The studies of the origin and source of formation water are still insufficient due to the complexity of relationship between gas and formation water. Based on the analysis of major components, trace elements, as well as hydrogen and oxygen isotopes, the indication of geochemical characteristics for the source of formation water is then revealed. The Permian formation water in Hangjinqi area is mainly of CaCl₂ type, and the average total dissolved solids (TDS) of formation water to the north and south of the Borjianghaizi fault are 52.1 and 41.9 g/L, respectively. Different water chemical parameters indicate favorable formation sealing conditions, and the formation water has experienced strong concentrated metamorphism with beneficial preservation conditions for natural gas. The formation water is mainly terrigenous one after evaporation and concentration, and the stratum has experienced albitization of plagioclase and dolomitization of cements. The δD and δ¹⁸O values of the formation water are mainly in the ranges of -81‰ to -75‰ and -12.1‰ to -8.8‰, respectively, suggesting weaker water-rock interaction than that in the Sulige gas field. Due to the mixing of condensate water in regional uplift since the Late Cretaceous or the seepage of surface water along faults, a small number of formation water samples display more negative δD values.
- total dissolved solids /
- trace elements /
- hydrogen and oxygen isotopes /
- formation water /
- Permian /
- Hangjinqi area /
- Ordos Basin

HTML全文

图 1 鄂尔多斯盆北部杭锦旗地区构造位置(a)和井位分布(b)

Figure 1. Tectonic location (a) and distribution of gas wells (b) in Hangjinqi area, northern Ordos Basin

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图 2 鄂尔多斯盆地杭锦旗地区二叠系地层水Na⁺+K⁺(a)和Cl^-含量(b)与TDS相关图

苏里格气田数据据窦伟坦等^[15]。

Figure 2. Correlation diagrams of Na⁺+K⁺ contents (a) and Cl^- contents (b) versus TDS of Permian formation water from Hangjinqi area, Ordos Basin

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图 3 鄂尔多斯盆地杭锦旗地区二叠系地层水脱硫系数与钠氯系数(a)和盐化系数与变质系数(b)相关图

苏里格气田数据据窦伟坦等^[15]。

Figure 3. Correlation diagrams of desulfurization coefficient versus solium-chloride coefficient (a) and salinization coefficient versus metamorphic coefficient (b) of Permian formation water from Hangjinqi area, Ordos Basin

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图 4 鄂尔多斯盆地杭锦旗地区二叠系地层水Cl^-与Na⁺ (a)、Ca²⁺ (b)、Mg²⁺ (c)、Sr(d)含量相关图

底图据覃伟等^[16]；苏里格气田数据据窦伟坦等^[15]。

Figure 4. Correlation diagrams of Cl^- versus Na⁺ (a), Ca²⁺ (b), Mg²⁺ (c), and Sr(d) concentrations in Permian formation water from Hangjinqi area, Ordos Basin

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图 5 鄂尔多斯盆地杭锦旗地区二叠系地层水氢、氧同位素值相关图

苏里格气田数据据窦伟坦等^[15]；全球大气降水线据CRAIG^[45]。

Figure 5. Correlation diagrams of δD versus δ¹⁸O values of Permian formation water from Hangjinqi area, Ordos Basin

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表 1 鄂尔多斯盆地杭锦旗地区地层水矿化度、微量元素含量和氢、氧同位素组成

Table 1. Total dissolved solids (TDS), trace element concentrations, and hydrogen and oxygen isotopic compositions of formation water from Hangjinqi area, Ordos Basin

区带	井号	地层	矿化度/(g·L^-1)	pH	水型	微量元素含量/(mg·L^-1)				δD/‰	δ¹⁸O/‰
区带	井号	地层	矿化度/(g·L^-1)	pH	水型	Sr	Ba	Mn	B	δD/‰	δ¹⁸O/‰
什股壕	JPH-13	P₁x	61.6	5.9	CaCl₂	871	300	29.44	8.18	-77	-9.2
	J66	P₁x	61.4	5.9	CaCl₂	866	141	19.75	13.41	-80	-4.0
	J11P4H	P₁x	54.6	6.4	CaCl₂	716	260	9.13	5.80	-81	-9.8
	ESP2	P₁x	45.7	6.5	CaCl₂	568	176	10.84	8.74	-81	-9.5
	JPH-1	P₁x	51.8	6.9	CaCl₂	826	237	19.88	9.99	-77	-9.5
	JPH-2	P₁x	52.9	6.1	CaCl₂	870	301	18.96	8.26	-76	-8.8
	J11-2	P₁x	45.2	6.3	CaCl₂	561	175	10.35	8.92	-81	-9.7
	ES4	P₁x	16.8	7.2	CaCl₂	212	66	3.49	3.92	-103	-9.3
独贵加汗	J110	P₁x	46.0	6.9	CaCl₂	724	77	23.45	33.56	-129	-12.1
	J111	P₁x	44.4	5.9	CaCl₂	749	37	8.73	10.77	-76	-9.3
	J58P13H	P₁x	32.5	6.6	CaCl₂	479	71	13.13	22.77	-75	-9.8
十里加汗	J104	P₁s	28.1	7.8	CaCl₂	478	569	1.99	17.52	-76	-10.2

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