川西北地区中二叠统栖霞组白云岩形成机理——以车家坝剖面为例

曾杰; 董少峰

doi:10.11781/sysydz202402288

川西北地区中二叠统栖霞组白云岩形成机理——以车家坝剖面为例

doi: 10.11781/sysydz202402288

曾杰,
董少峰^,

西南石油大学地球科学与技术学院, 成都 610500

基金项目:

国家自然科学基金面上基金 42072139

详细信息

作者简介:
曾杰(1999—)，男，硕士生，沉积学(含古地理学)专业。E-mail: Zengjie_0712@163.com

通讯作者:
董少峰(1983—)，男，副研究员，硕士生导师，从事碳酸盐岩沉积成储的基础理论和应用研究。E-mail：dsf8332@163.com

中图分类号: TE122.21
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- 被引次数: 0
出版历程
- 收稿日期: 2023-10-17
- 修回日期: 2024-02-23
- 刊出日期: 2024-03-28

Origin of dolomite in Middle Permian Qixia Formation in northwestern Sichuan Basin: a case study of Chejiaba section

ZENG Jie,
DONG Shaofeng^,

School of Geoscience and Technology, Southwest Petroleum University, Chengdu, Sichuan 610500, China

摘要

摘要: 以岩石学观察为基础，结合稳定同位素与团簇同位素分析，探讨了川西北地区中二叠统栖霞组白云岩形成机理。川西北车家坝剖面白云岩集中发育于栖霞组上段，可识别出基质白云石与白云石胶结物2种不同类型的白云石。基质白云岩呈灰白色，与灰岩接触界线截然，呈指状交错接触；白云石胶结物呈乳白色，局限分布于溶蚀孔洞的边缘。镜下可进一步划分为3种类型基质白云石，即漂浮状细晶直面自形—半自形基质白云石(Md1)、细—中晶直面自形—半自形基质白云石(Md2)、中—粗晶它形曲面基质白云石(Md3)，以及一种鞍形白云石胶结物(Sd)。Md1沿缝合线呈漂浮状分布于灰泥基质中，可能为浅埋藏环境下压溶作用的产物。Md2与Md3具有与宿主灰岩相似的δ¹³C、δ¹⁸O和⁸⁷Sr/⁸⁶Sr同位素特征，指示白云石化流体主要来源于二叠纪同期海水，而相对较高的成岩温度说明受二叠纪末大规模火山活动的影响显著。鞍形白云石及其后的方解石胶结物具有明显偏负的δ¹⁸O值和放射性⁸⁷Sr/⁸⁶Sr值，说明它们形成于高温外源富放射性锶的白云石化流体中，可能为来自或穿过碎屑岩地层的深部热流体。川西北地区栖霞组白云岩的形成受原始沉积相与断裂活动的双重控制，热流体的注入使原始滩相地层发生白云石化作用，形成大量溶洞与晶间溶孔，对储层的改造起到了积极的建设性作用。
- 热流体 /
- 稳定同位素 /
- 团簇同位素 /
- 白云岩 /
- 栖霞组 /
- 中二叠统 /
- 川西北地区
Abstract: This study focuses on the origin of dolomite within the Middle Permian Qixia Formation in the northwestern Sichuan Basin by the approaches of petrographic examination and stable isotopic as well as clumped isotopic analysis. Two types of dolomite (matrix dolomite and dolomite cement) in the upper part of the Qixia Formation at the Chejiaba (CJB) section were classified. The gray matrix dolomite shows a clear inter-finger contact with limestone, while the milky white dolomite cement lines the edges of dissolved pores. Microscopic examination revealed three types of matrix dolomite including floating fine crystalline, planar-e(s) matrix dolomite (Md1); fine to medium crystalline, planar-e(s) matrix dolomite (Md2); and medium to coarse crystalline, planar-a matrix dolomite (Md3), along with saddle dolomite cement (Sd). The presence of Md1 dolomites along stylolites suggests they were formed due to pressure dissolution during shallow burial. The similar isotopic signatures of Md2 and Md3 with the host limestone indicate that the dolomitizing fluids likely originated from Permian seawater. However, elevated diagenetic temperatures suggest an influence from the Late Permian volcanic activity. The Sd dolomite and subsequent calcite cementation with negative δ¹⁸O values and radioactive ⁸⁷Sr/⁸⁶Sr ratios point to formation in high-temperature, externally-derived, radio-genic strontium-rich dolomitizing fluids, possibly from deep-seated thermal fluids within siliciclastic strata. The formation of dolomite in the Qixia Formation of the northwestern Sichuan Basin was influenced by both original sedimentary facies and faulting activities. The influx of hydrothermal fluids triggered widespread dolomitization, resulting in the creation of numerous dissolved and inter-crystalline pores, which played a beneficial role in reservoir development.
- hydrothermal fluid /
- stable isotope /
- clumped isotope /
- dolomite /
- Qixia Formation /
- middle Permian /
- northwestern Sichuan Basin
注释:

利益冲突声明/Conflict of Interests

所有作者声明不存在利益冲突。

All authors disclose no relevant conflict of interests.

作者贡献/Authors’Contributions

所有野外样品采集、室内岩石学与地球化学分析均由董少峰与曾杰共同完成，此外，曾杰负责论文初稿的撰写，董少峰负责审阅与修改。所有作者均阅读并同意最终稿件的提交。

All the sample collection, petrological examination and geochemical analysis were carried out by DONG Shaofeng and ZENG Jie. In addition, the manuscript was drafted by ZENG Jie and revised by DONG Shaofeng. All the authors have read the last version of paper and consented for submission.

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图 1 川西北地区地质背景

a.车家坝剖面大地构造位置(改自邓小亮等^[17])；b.车家坝剖面地层柱状图。

Figure 1. Geological settings of northwestern Sichuan Basin

下载: 全尺寸图片幻灯片

图 2 川西北地区K2井埋藏热史及古热流趋势

红色为栖霞组；据DONG等^[11]。

Figure 2. Burial history and paleoheat flow distribution of well K2 in northwestern Sichuan Basin

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图 3 川西北地区车家坝剖面栖霞组下段宿主灰岩岩石学特征

a.灰色中层粒泥灰岩与深灰色泥灰岩互层；b.泥灰岩中生物定向性排列；c.粒泥灰岩中单体珊瑚原始结构保存良好，被沥青浸染的微裂缝发育；d.粒泥灰岩镜下特征，单偏光；e.泥灰岩中生屑定向性排列，微裂缝与缝合线大量发育并被沥青充填，正交偏光；f.生屑颗粒中世代方解石胶结物，并被缝合线切割，正交偏光；g.生屑颗粒丰富，颗粒间灰泥支撑，灰泥基质与生屑颗粒发极暗红色光；h.泥灰岩阴极发光特征与粒泥灰岩相似，发极暗红色光。

Figure 3. Petrology characteristics of host limestone in lower part of Qixia Formation, Chejiaba section, northwestern Sichuan Basin

下载: 全尺寸图片幻灯片

图 4 川西北地区车家坝剖面栖霞组Md1白云石宏、微观特征

a.灰岩与白云岩呈指状交错接触，局部含有残留的原始灰岩(黄色圈)；b.孔洞被沥青与鞍形白云石充填(黄色箭头)；c.Md1间呈点—线接触或漂浮状分布，雾心亮边特征明显，正交偏光；d.为图c中的红框放大部位，Md1沿缝合线发育，正交偏光；e.自形程度相对较差的Md1晶体间呈晶簇状分布，单偏光；f.Md1发环带状红光。

Figure 4. Macro- and microscopic characteristics of Md1 dolomite of Qixia Formation in Chejiaba section, northwestern Sichuan Basin

下载: 全尺寸图片幻灯片

图 5 川西北地区车家坝剖面栖霞组Md2岩石学特征

a.Md2呈自形—半自形结构，晶体间为点—线接触，与Md3呈过渡接触，单偏光；b.Md2晶体间孔隙发育，以平直晶面晶间孔为主(黄色箭头)，单偏光；c.Md2被缝合线(白色箭头)切割，单偏光；d.Md2呈环带状发光，与Md1类似。

Figure 5. Petrology characteristics of Md2 dolomite of Qixia Formation in Chejiaba section, northwestern Sichuan Basin

下载: 全尺寸图片幻灯片

图 6 川西北地区车家坝剖面栖霞组Md3与缝洞充填物(Sd与Cc)的岩石学特征

a.Md3晶面弯曲、浑浊，晶体间呈镶嵌状接触，溶蚀孔发育，单偏光；b.Md3具明显波状消光特征，正交偏光；c.溶蚀孔洞被鞍形白云石与方解石完全充填，鞍形白云石被沥青浸染，单偏光；d.图c的正交偏光特征；e.Md3、Sd与Cc共生关系，单偏光；f.Sd发红光，Cc不发光，Md3发暗红光—不发光。

Figure 6. Petrographic characteristics of Md3 dolomite and subsequent fracture and vug fillings (Sd and Cc) of Qixia Formation in Chejiaba section, northwestern Sichuan Basin

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图 7 川西北地区车家坝剖面不同类型样品碳氧同位素(a)与锶同位素(b)特征

图中蓝色区域为中二叠世海水碳氧同位素与锶同位素范围。

Figure 7. Carbon and oxygen isotope (a) and strontium isotope (b) characteristics of different types of samples from Chejiaba section, northwestern Sichuan Basin

下载: 全尺寸图片幻灯片

图 8 川西北中二叠统栖霞组白云岩成因模式示意

改自DONG等^[11]与韩月卿等^[40]。

Figure 8. Genetic model of dolomite of Middle Permian Qixia Formation in northwestern Sichuan Basin

下载: 全尺寸图片幻灯片

表 1 川西北地区车家坝剖面与K2井栖霞组不同类型碳酸盐岩地球化学分析测试结果

Table 1. Geochemical analytical results of different types of carbonates from Qixia Formation in Chejiaba section and well K2, northwestern Sichuan Basin

样品号	测试类型	δ¹³C_VPDB/‰	δ¹⁸O_VPDB/‰	Δ₄₇/‰	T_Δ47 /℃	⁸⁷Sr/⁸⁶Sr
CJB-01	宿主灰岩	2.89	-5.02
CJB-17	宿主灰岩	2.84	-4.66
CJB-48	宿主灰岩	2.97	-8.25	0.595 7	52.3	0.707 6
CJB-60	宿主灰岩	0.57	-7.87	0.593 3	53.0	0.707 5
CJB-105	宿主灰岩	2.49	-7.45
CJB-60	Md1	1.45	-8.20
CJB-105	Md1	3.14	-4.77			0.707 2
CJB-67	Md2	2.81	-7.18	0.549 9	65.5	0.707 6
CJB-72	Md2	2.79	-7.71
CJB-56	Md2	2.52	-7.84			0.707 5
CJB-97	Md2	2.69	-6.69
CJB-87	Md2	2.68	-6.66	0.562 5	61.7	0.707 4
CJB-58	Md3	2.70	-6.39
CJB-76	Md3	2.46	-7.80			0.707 5
CJB-80	Md3	2.58	-6.72			0.707 4
CJB-92	Md3	2.30	-6.78	0.515 3	76.6	0.707 4
CJB-99	Md3	2.79	-7.11
K2-22	Sd	1.01	-16.35			0.709 8
K2-11	Sd	1.03	-14.18			0.709 7
CJB-59	Cc	-1.71	-11.55			0.708 9
CJB-92	Cc	-5.48	-15.49	0.569 2	59.7	0.708 7
注：K2-22、K2-11鞍形白云石数据来源于PAN等^[30]。

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