塔河地区下奥陶统蓬莱坝组白云岩特征与成因分析

徐勤琪; 彭军; 何成其; 夏金刚; 刘瑞; 黄苇

doi:10.11781/sysydz2025040805

塔河地区下奥陶统蓬莱坝组白云岩特征与成因分析

doi: 10.11781/sysydz2025040805

徐勤琪^1,,
彭军^{2, 3},
何成其^2, ,,
夏金刚²,
刘瑞¹,
黄苇¹

1.
中国石化西北油田分公司勘探开发研究院, 乌鲁木齐 830011
2.
西南石油大学地球科学与技术学院, 成都 610500
3.
天然气地质四川省重点实验室, 成都 610500

基金项目:

中国石化西北油田分公司勘探开发研究院测试分析项目“塔里木盆地碳酸盐岩储层发育机理与重点区带评价方法” 34400008-22-ZC0613-0064

详细信息

作者简介:
徐勤琪(1985—)，男，副研究员，从事石油地质与油气成藏研究工作。E-mail: xuqq.xbsj@sinopec.com

通讯作者:
何成其(1997—)，男，硕士生，从事碳酸盐岩沉积学研究。E-mail: 1804873167@qq.com

中图分类号: TE122.2
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- 被引次数: 0
出版历程
- 收稿日期: 2024-04-20
- 修回日期: 2025-05-15
- 刊出日期: 2025-07-28

Characteristics and genesis analysis of dolomite in Lower Ordovician Penglaiba Formation in Tahe area

XU Qinqi^1
,,
PENG Jun^{2, 3},
HE Chengqi^{2
, ,},
XIA Jingang²,
LIU Rui¹,
HUANG Wei¹

1.
Exploration and Production Research Institute, Northwest Oilfield Company, SINOPEC, Urumqi, Xinjiang 830011, China
2.
School of Geoscience and Technology, Southwest Petroleum University, Chengdu, Sichuan 610500, China
3.
Sichuan Provincial Key Laboratory of Natural Gas Geology, Chengdu, Sichuan 610500, China

摘要

摘要: 下奥陶统蓬莱坝组白云岩是塔河油田油气勘探的重要接替领域，明确白云岩的沉积特征、成因机理对塔河油田的油气勘探与开发具有重要意义。综合岩心描述、薄片鉴定、扫描电镜、阴极发光及地球化学等分析手段，系统研究了塔河油田下奥陶统蓬莱坝组白云岩的地质地球化学特征及成因机制。结果表明：(1)研究区以晶粒白云岩为主，残余颗粒白云岩次之。泥—微晶白云石以他形为主，粉—中晶多呈半自形—自形，中—粗晶以异形为主；残余颗粒白云岩以粉—细晶为主，可见残余内碎屑结构。(2)阴极发光显示：泥—微晶呈暗淡蓝紫或暗褐色光；粉晶为暗淡紫红色；细—中晶具紫色核心、橙红色亮边环带结构；中—粗晶呈紫红与明亮棕红色环带发光。(3)泥—微晶白云岩主要为重稀土富集，δ¹⁸O值波动大，⁸⁷Sr/⁸⁶Sr值接近早奥陶世海水值，指示高盐度蒸发海水的准同生白云石化作用；残余颗粒白云岩主要为残余内碎屑结构，属埋藏云化成因；粉晶白云岩、细—中晶白云岩稀土元素(REE)配分模式与同期泥晶灰岩类似，重稀土富集，δ¹⁸O值跨度较大，⁸⁷Sr/⁸⁶Sr值部分高于同期海水锶同位素值，为浅—中埋藏云化叠加热液改造的产物；中—粗晶白云岩轻稀土相对富集，δ¹⁸O值偏负，⁸⁷Sr/⁸⁶Sr值高于同期海水值，属碎屑岩层热液交代成因。
- 白云岩 /
- 成因机理 /
- 蓬莱坝组 /
- 下奥陶统 /
- 塔河油田
Abstract: The dolomite of the Lower Ordovician Penglaiba Formation is an important successor field for oil and gas exploration in the Tahe oilfield. Clarifying the sedimentary characteristics and genetic mechanisms of the dolomite is of great significance for oil and gas exploration and development in the Tahe oilfield. Based on this, the geological and geochemical characteristics and genetic mechanisms of the dolomite in the Lower Ordovician Penglaiba Formation of the Tahe Oilfield were systematically studied through core description, thin section identification, scanning electron microscopy, cathodoluminescence, and geochemical analyses. The results showed that: (1) The study area was dominated by crystalline dolomite, followed by residual granular dolomite. Mud-microcrystalline dolomite was mainly anhedral. Silty-medium crystalline dolomite was mostly subhedral to euhedral. Medium-coarse crystalline dolomite was predominantly xenomorphic. Residual granular dolomite was mainly composed of silty-fine crystalline dolomite, showing residual intraclastic texture. (2) Cathodoluminescence showed that the mud- microcrystalline dolomite emitted dull blue-purple or dark brown luminescence. Silty dolomite emitted dull purple-red luminescence. Fine-medium crystalline dolomite had a purple core with a bright orange-red rim-shaped band. Medium-coarse crystalline dolomite exhibited purple-red and a bright brown-red rim-shaped luminescent band. (3) Mud-microcrystalline dolomite was mainly enriched in heavy rare earth elements (REE), with large δ¹⁸O fluctuations and ⁸⁷Sr/⁸⁶Sr ratios close to those in the Early Ordovician seawater, indicating quasi-syngenetic dolomitization by high-salinity evaporative seawater. Residual granular dolomite was mainly characterized by residual intraclastic texture and its genetic mechanism was burial dolomitization. The REE distribution patterns of silty crystalline dolomite and fine-medium crystalline dolomite were similar to those of contemporaneous micrites, which were enriched in heavy REEs with large δ¹⁸O fluctuations. The ⁸⁷Sr/⁸⁶Sr values were partially higher compared with the strontium isotope values in contemporaneous seawater, indicating products of shallow-medium burial dolomitization superimposed with hydrothermal fluids. Medium-coarse crystalline dolomite was relatively enriched in light rare earth, with negative δ¹⁸O values and ⁸⁷Sr/⁸⁶Sr values higher than those in contemporaneous seawater, indicating formation by hydrothermal metasomatism related to clastic rock layers.
- dolomite /
- genetic mechanism /
- Penglaiba Formation /
- Lower Ordovician /
- Tahe Oilfield
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 declare no relevant conflict of interests.

作者贡献/Authors'Contributions

徐勤琪、彭军、何成其、夏金刚、刘瑞、黄苇参与实验设计、论文写作和修改。所有作者均阅读并同意最终稿件的提交。

XU Qinqi, PENG Jun, HE Chengqi, XIA Jingang, LIU Rui and HUANG Wei participated in the experimental design, paper preparation, and revision. All authors have read the final version of the paper and consented to its submission.

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图 1 塔里木盆地构造单元划分(a)、研究区构造位置(b)、研究区蓬莱坝组岩性地层综合柱状图(c)

Figure 1. Tectonic unit division in Tarim Basin (a), tectonic location of study area (b), and comprehensive lithostratigraphic column of Penglaiba Formation in study area (c)

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图 2 塔河地区奥陶系蓬莱坝组残余颗粒白云岩、泥—微晶白云岩岩石学特征

a.残余砂屑白云岩，S88井，6 552.61~6 552.70 m，表面呈深浅不一的斑块状，岩心照片；b.残余颗粒白云岩，TS2井，6 551.13 m铸体薄片，残余颗粒结构，可见多个颗粒幻影；c.残余砂屑白云岩，TS2井，6 550.55 m，见砂屑幻影，颗粒边缘清晰，原岩是亮晶砂屑灰岩，胶结物被晶粒更大的白云石所交代；d.残余砂屑白云岩，与c同视域，TS2井，6 650.55 m，颗粒发暗红色光—暗紫色光，胶结物发暗紫色光，阴极发光照片；e.微晶白云岩，S88井，6 564.20~6 564.28 m，块状构造，岩心照片；f.泥—微晶白云岩，TS2井，6 694.10 m，微晶结构；g.微晶白云岩，TS2井，6 553.08 m，扫描电镜，半自形，白云石晶间孔充填片状伊蒙混层；h.泥—微晶白云岩，与f同视域，6 694.10 m，阴极发光照片，基质泥—微晶白云石发暗淡的紫红色光。

Figure 2. Petrographic characteristics of residual granular dolomite and mud-microcrystalline dolomite of Ordovician Penglaiba Formation in Tahe area

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图 3 塔河地区奥陶系蓬莱坝组晶粒白云岩岩石学特征

a.粉晶白云岩，TS2井，6 554.12~6 554.17 m，可见灰黑色沥青质，及部分后期充填形成的白云石，岩心照片；b.微—粉晶白云岩，TS2井，6 691.39 m，晶面浑浊，裂缝由白云石充填；c.粉晶白云岩，TS2井，6 691.84 m，自形，晶间见伊蒙混层充填，扫描电镜；d.微—粉晶白云岩，与b同视域，TS2井，6 691.39 m，基质白云石发红紫色光，裂缝中充填的白云石中央部位发红紫色光，边缘部位发较明亮的橙红色光，阴极发光；e.细晶白云岩，TS2井，6 555.10~6 555.16 m，发育深灰色纹层状构造，岩心照片；f.细晶白云岩，TS2井，6 651.32 m；g.细晶白云岩，TS2井，6 694.91 m，自形直面接触，扫描电镜；h.细—中晶白云岩，与f同视域，TS2井，6 651.32 m，白云石发光具暗蓝紫色核心和橙红色亮边环带结构，阴极发光；i.中—粗晶鞍形白云石，S88井，6 368.48 m，残余晶间孔，白云石晶粒受成岩改造，已无法分辨晶粒边界，晶面浑浊，铸体薄片；j. 裂缝边缘充填粗晶鞍形白云石，TS2井，6 691.84 m，裂缝中心充填粗晶方解石；k.中—粗晶鞍形白云石，S88井，6 562.25 m，自形程度差，晶体间曲面接触，扫描电镜；l.粗晶鞍形白云石，与j同视域，TS2井，6 691.84 m，白云石核部发紫红色光，边缘发亮红色光，裂缝中心充填方解石发棕色光，阴极发光。

Figure 3. Petrographic characteristics of crystalline dolomite in Ordovician Penglaiba Formation of Tahe area

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图 4 塔河地区奥陶系蓬莱坝组白云岩碳氧同位素值散点图

Figure 4. Scatter plots of carbon and oxygen isotope values of dolomite from Ordovician Penglaiba Formation in Tahe area

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图 5 塔河地区奥陶系蓬莱坝组白云岩锶同位素值散点图

Figure 5. Scatter plots of strontium isotope values of dolomite from Ordovician Penglaiba Formation in Tahe area

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图 6 塔河地区奥陶系蓬莱坝组白云岩稀土元素配分模式

Figure 6. Rare earth element distribution patterns of dolomite from Ordovician Penglaiba Formation in Tahe area

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图 7 塔河地区奥陶系蓬莱坝组白云岩发育模式

Figure 7. Dolomite development pattern of Ordovician Penglaiba Formation in Tahe area

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表 1 塔河地区奥陶系蓬莱坝组白云岩碳氧同位素值

Table 1. Carbon and oxygen isotope values of dolomite from Ordovician Penglaiba Formation in Tahe area

井号	深度/m	岩性	δ¹³C_V-PDB/‰	δ¹⁸O_V-PDB/‰
TS2	6 550.14	泥—微晶白云岩	-0.90	-8.10
TS2	6 550.77	泥—微晶白云岩	-1.20	-7.20
TS2	6 551.88	泥—微晶白云岩	-0.70	-7.60
TS2	6 552.35	泥—微晶白云岩	-1.10	-8.40
TS2	6 552.75	泥—微晶白云岩	-0.80	-6.50
TS2	6 552.93	泥—微晶白云岩	-0.80	-8.30
TS2	6 553.72	泥—微晶白云岩	-1.20	-6.00
TS2	6 694.00	泥—微晶白云岩	-1.10	-7.30
TS2	6 694.80	泥—微晶白云岩	-1.20	-6.30
S88	6 423.03	粉晶白云岩	-1.57	-9.12
S88	6 453.15	粉晶白云岩	-1.55	-4.26
TS2	6 550.77	粉晶白云岩	-1.40	-7.30
TS2	6 551.79	粉晶白云岩	-1.00	-9.40
TP193	7 466.79	粉晶白云岩	-1.67	-4.23
TP193	7 471.55	粉晶白云岩	-1.22	-4.40
S88	6 423.03	粉晶白云岩	-1.57	-9.12
S88	6 337.15	细—中晶白云岩	-1.79	-7.58
S88	6 423.24	细—中晶白云岩	-1.96	-5.32
S88	6 457.13	细—中晶白云岩	-1.48	-8.78
TS2	6 550.84	细—中晶白云岩	-1.72	-6.63
S88	6 562.14	细—中晶白云岩	-1.39	-6.96
TP193	7 368.62	细—中晶白云岩	-1.24	-8.12
TP193	7 466.79	细—中晶白云岩	-1.89	-7.77
TP193	7 471.76	细—中晶白云岩	-1.62	-9.86
S88	6 368.71	中—粗晶白云岩	-1.40	-9.70
S88	6 428.80	中—粗晶白云岩	-1.30	-8.90
TS2	6 694.57	中—粗晶白云岩	-1.00	-8.40
TP193	7 472.81	中—粗晶白云岩	-1.30	-8.30
TS6	7 690.15	中—粗晶白云岩	-1.60	-8.90

下载: 导出CSV

表 2 塔河地区奥陶系蓬莱坝组白云岩锶同位素值

Table 2. Strontium isotope values of dolomite from Ordovician Penglaiba Formation in Tahe area

井号	深度/m	岩性	⁸⁷Sr/⁸⁶Sr
S88	6 485.00	泥—微晶白云岩	0.709 046
S88	6 518.98	泥—微晶白云岩	0.709 023
TS2	6 550.61	泥—微晶白云岩	0.709 009
TS2	6 550.77	泥—微晶白云岩	0.708 926
S88	6 557.13	泥—微晶白云岩	0.708 999
TS2	6 691.84	泥—微晶白云岩	0.708 938
TS2	6 694.00	泥—微晶白云岩	0.709 005
TS2	6 694.80	泥—微晶白云岩	0.708 929
TS2	6 550.14	泥—微晶白云岩	0.708 789
TS2	6 550.55	泥—微晶白云岩	0.708 923
TS2	6 551.60	泥—微晶白云岩	0.708 887
TS2	6 551.88	泥—微晶白云岩	0.708 906
TS2	6 552.02	泥—微晶白云岩	0.708 949
TS2	6 552.35	泥—微晶白云岩	0.708 852
TS2	6 552.75	泥—微晶白云岩	0.708 920
TS2	6 552.93	泥—微晶白云岩	0.708 864
S88	6 485.00	粉晶白云岩	0.709 057
S88	6 519.20	粉晶白云岩	0.709 073
TS2	6 550.77	粉晶白云岩	0.708 924
TS2	6 551.79	粉晶白云岩	0.709 213
TS2	6 691.55	粉晶白云岩	0.709 020
TP193	7 468.86	粉晶白云岩	0.709 075
TP193	7 517.00	粉晶白云岩	0.708 853
TS6	7 561.49	粉晶白云岩	0.708 716
TS6	7 619.92	粉晶白云岩	0.708 825
TS6	7 691.86	粉晶白云岩	0.709 076
TS2	6 552.29	细—中晶白云岩	0.709 204
TS2	6 694.39	细—中晶白云岩	0.709 429
TP193	7 471.76	细—中晶白云岩	0.709 205
TP193	7 472.80	细—中晶白云岩	0.709 145
TS6	7 521.71	细—中晶白云岩	0.709 419
TP193	7 530.00	细—中晶白云岩	0.709 260
TS6	7 690.15	细—中晶白云岩	0.709 245
TS6	7 690.66	细—中晶白云岩	0.709 553
TS6	7 691.99	细—中晶白云岩	0.709 688
S88	6 367.05	中—粗晶白云岩	0.709 182
S88	6 368.46	中—粗晶白云岩	0.709 317
S88	6 428.80	中—粗晶白云岩	0.709 435
TS2	6 694.57	中—粗晶白云岩	0.709 219
TP193	7 471.76	中—粗晶白云岩	0.709 244
TP193	7 517.00	中—粗晶白云岩	0.709 262

下载: 导出CSV

表 3 塔河地区奥陶系蓬莱坝组白云岩稀土元素数据

Table 3. Rare earth element data of dolomite from Ordovician Penglaiba Formation in Tahe area μg/g

井号	井深/m	岩性	La	Ce	Pr	Nd	Sm	Eu	Gd	Tb	Dy	Ho	Er	Tm	Yb	Lu
S88	6 369.15	泥晶灰岩	2.504	3.792	0.565	2.345	0.466	0.036	0.418	0.054	0.379	0.130	0.179	0.040	0.193	0.035 0
S88	6 369.40	泥晶灰岩	2.215	2.882	0.421	1.796	0.328	0.046	0.364	0.044	0.272	0.111	0.127	0.033	0.135	0.027 0
TS2	6 550.14	泥—微晶白云岩	1.310	2.240	0.242	0.871	0.157	0.031	0.144	0.024	0.120	0.022	0.061	0.010	0.071	0.009 0
TS2	6 551.60	泥—微晶白云岩	1.510	2.970	0.309	1.200	0.236	0.050	0.200	0.038	0.208	0.039	0.113	0.018	0.116	0.017 0
TS2	6 551.88	泥—微晶白云岩	0.925	1.610	0.176	0.648	0.118	0.025	0.117	0.020	0.115	0.021	0.058	0.010	0.061	0.016 0
TS2	6 552.93	泥—微晶白云岩	0.884	1.600	0.176	0.673	0.125	0.019	0.114	0.020	0.109	0.020	0.055	0.010	0.064	0.015 0
TS2	6 552.02	泥—微晶白云岩	1.380	2.560	0.265	1.020	0.195	0.035	0.175	0.032	0.170	0.031	0.087	0.013	0.093	0.014 0
TS2	6 552.35	泥—微晶白云岩	1.290	2.280	0.255	0.940	0.175	0.031	0.151	0.026	0.140	0.024	0.070	0.011	0.081	0.011 0
S88	6 421.23	粉晶白云岩	1.200	2.100	0.130	0.500	0.110	0.060	0.110	0.010	0.110	0.020	0.090	0.010	0.030	0.012 0
S88	6 453.15	粉晶白云岩	0.900	2.200	0.270	1.000	0.190	0.080	0.160	0.030	0.170	0.030	0.140	0.008	0.090	0.009 0
TS2	6 551.79	粉晶白云岩	0.400	0.900	0.090	0.300	0.060	0.040	0.070	0.010	0.120	0.025	0.060	0.008	0.030	0.009 0
TS2	6 551.79	粉晶白云岩	1.000	1.800	0.250	1.000	0.180	0.070	0.160	0.020	0.130	0.030	0.070	0.010	0.070	0.011 0
TS2	6 691.55	粉晶白云岩	0.800	2.100	0.270	1.000	0.160	0.070	0.140	0.020	0.150	0.030	0.120	0.009	0.070	0.014 0
TP193	7 466.79	粉晶白云岩	1.000	2.500	0.290	1.100	0.180	0.100	0.160	0.020	0.100	0.030	0.150	0.009	0.080	0.010 0
TP193	7 470.55	粉晶白云岩	1.000	2.700	0.310	1.100	0.190	0.090	0.190	0.030	0.250	0.040	0.180	0.008	0.070	0.012 0
S88	6 337.15	细—中晶白云岩	0.500	1.600	0.200	0.700	0.110	0.050	0.110	0.010	0.160	0.020	0.090	0.009	0.050	0.008 0
S88	6 423.24	细—中晶白云岩	0.400	2.300	0.150	0.500	0.080	0.050	0.090	0.020	0.090	0.020	0.070	0.008	0.050	0.009 0
TS2	6 550.77	细—中晶白云岩	0.200	0.700	0.100	0.400	0.030	0.030	0.060	0.010	0.050	0.010	0.030	0.009	0.020	0.009 8
TS2	6 550.84	细—中晶白云岩	0.300	2.800	0.320	1.100	0.200	0.110	0.200	0.030	0.120	0.040	0.190	0.009	0.090	0.008 9
S88	6 562.14	细—中晶白云岩	0.600	1.600	0.220	0.700	0.130	0.060	0.100	0.020	0.170	0.020	0.100	0.008	0.060	0.008 4
TP193	7 471.76	细—中晶白云岩	0.500	1.500	0.110	0.400	0.090	0.050	0.060	0.010	0.090	0.010	0.070	0.010	0.030	0.007 5
TP193	7 472.81	细—中晶白云岩	0.300	1.500	0.180	0.700	0.130	0.070	0.110	0.020	0.160	0.030	0.100	0.009	0.060	0.006 8
S88	6 368.71	中—粗晶白云岩	0.588	1.270	0.125	0.476	0.093	0.018	0.094	0.014	0.077	0.016	0.043	0.006	0.038	0.006 0
S88	6 428.80	中—粗晶白云岩	0.610	1.160	0.123	0.454	0.088	0.020	0.081	0.011	0.061	0.012	0.035	0.005	0.030	0.005 0
TS2	6 694.57	中—粗晶白云岩	0.570	1.230	0.126	0.482	0.095	0.019	0.096	0.014	0.078	0.016	0.043	0.006	0.038	0.006 0
TS6	7 690.15	中—粗晶白云岩	0.574	1.090	0.112	0.448	0.095	0.021	0.095	0.013	0.066	0.012	0.033	0.005	0.028	0.004 0
TS6	7 690.66	中—粗晶白云岩	0.673	1.280	0.138	0.513	0.098	0.019	0.092	0.014	0.076	0.015	0.042	0.006	0.037	0.006 0

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表 4 塔河奥陶系蓬莱坝组不同岩性的La_SN/Yb_SN、δCe、δEu特征

Table 4. La_SN/Yb_SN, δCe, and δEu characteristics of different lithologies of Ordovician Penglaiba Formation in Tahe area

岩性	La_SN/Yb_SN			δCe			δEu
岩性	最小值	最大值	平均值	最小值	最大值	平均值	最小值	最大值	平均值
泥晶灰岩	0.797	0.831	0.813	0.81	0.84	0.82	0.42	0.73	0.58
泥—微晶白云岩	0.812	1.261	0.989	0.95	1.08	1.00	0.74	1.04	0.92
粉晶白云岩	0.569	0.976	0.879	0.83	1.79	1.02	2.07	3.21	2.62
细—中晶白云岩	0.599	0.856	0.774	0.67	1.48	1.00	2.29	3.52	2.79
中—粗晶白云岩	1.034	1.274	1.149	1.00	1.12	1.06	1.02	1.14	1.13

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