黔东北梵净山地区沥青Re-Os同位素年龄对油气成藏年代的约束

于宁; 彭伟; 陈友智; 马明哲

doi:10.19509/j.cnki.dzkq.2021.0505

黔东北梵净山地区沥青Re-Os同位素年龄对油气成藏年代的约束

doi: 10.19509/j.cnki.dzkq.2021.0505

于宁^1,,
彭伟²,
陈友智^1, ,,
马明哲³

基金项目:

贵州省科技计划项目"黔北地区寒武系牛蹄塘组页岩气成藏条件及关键控制因素研究" 黔科合JZ字[2015]2005

贵州理工学院校立项目"华北板块南缘长城纪裂谷沉积的黑色页岩Re-Os同位素约束及油气地质意义"

详细信息

作者简介:
于宁(1980-), 男, 高级工程师, 主要从事构造地质学研究。E-mail: 1041171774@qq.com

通讯作者:
陈友智(1982-), 男, 讲师, 主要从事构造地质学、石油地质学研究。E-mail: cugchenyz@126.com

中图分类号: P632⁺.7
计量
- 文章访问数: 500
- PDF下载量: 305
- 被引次数: 0
出版历程
- 收稿日期: 2020-09-21

Constraint of the isotopic age of asphalt Re-Os on the age of hydrocarbon accumulation in Fanjingshan area in Northeast Guizhou

Yu Ning^1
,,
Peng Wei²,
Chen Youzhi^{1
, ,},
Ma Mingzhe³

摘要

摘要: 黔东北梵净山地区位于雪峰隆起西缘，前寒武纪-早古生代黑色有机质岩系发育，沥青显示广泛。该区在新元古代-中生代经历了晋宁期、加里东期及印支期-燕山期多幕构造变形，前人对后两期构造与油气成藏的响应关系研究较多，而关于晋宁期构造与油气成藏之间的匹配关系则鲜有报道。选取黔东北梵净山地区宝塔组灰岩溶蚀孔、洞内的沥青开展了Re-Os同位素研究，测试结果显示等时线年龄为（915±129）Ma。结合区域地质分析表明，梵净山地区存在晋宁期原生油藏，在加里东期被改造形成次生油藏，古隆起控制了次生油气藏的分布。本研究丰富了雪峰隆起西缘油气成藏期次，同时也促进了复杂构造变形条件下次生油气藏成藏机理研究，对我国南方新元古界油气勘探有重要意义。
- Re-Os同位素 /
- 沥青 /
- 晋宁期 /
- 宝塔组 /
- 雪峰隆起
Abstract: Fanjingshan area in Northeast Guizhou is located at the northern margin of Xuefeng Uplift. The black organic rock series developed from Precambrian to Early Paleozoic, and the asphalt is widely displayed. The Neoproterozoic-Mesozoic period in this area experienced the Jinning period, Caledonian period and Indochina-Yanshan movement multi-stage tectonic deformation. Previous studies mostly focused on the response relationship between the structure and hydrocarbon accumulation in the latter two periods, while the matching relationship between the structure and hydrocarbon accumulation in the Jinning period has not been reported. In this paper, Re-Os isotopic study was carried out on bitumen in limestone dissolution cave of Baota Formation in Fanjingshan area. The isochronal age is (915±129)Ma. Combined with the regional geological analysis, it is concluded that there are primary oil reservoirs of Jinning period in Fanjingshan area, secondary oil reservoirs were formed in Caledonian period, whose distribution was controlled by paleouplift. In summary, this study enriches the oil and gas accumulation stages in the north margin of Xuefeng Uplift, and also promotes the study on the mechanism of secondary reservoir accumulation under complex tectonic deformation. It is of profound significance to the exploration of Neoproterozoic oil and gas in South China.
- Re-Os isotopic /
- asphalt /
- Jinning Period /
- Baota Formation /
- Xuefeng Uplift

HTML全文

图 1 研究区位置图(a)及采样区地质简图(b) (据文献[6, 16]修改)

Figure 1. Location map of the study area (a) and geological sketch of sampling area (b)

下载: 全尺寸图片幻灯片

图 2 被沥青充填的宝塔组灰岩“马蹄形”裂缝(a)和溶蚀洞(b)

Figure 2. "Horseshoe" fractures (a) and corroded cavities (b) filled with asphalt in limestone of the Baota Formation

下载: 全尺寸图片幻灯片

图 3 沥青样品Re-Os同位素等时线年龄

a.所有样品数据的等时线年龄；b.样品BT1、BT3、BT4和BT7所得到的等时线年龄；c.样品BT1、BT4和BT7所得到的等时线年龄

Figure 3. Re-Os isotope isochron age of asphalt samples

下载: 全尺寸图片幻灯片

图 4 梵净山地区晋宁期古油藏演化模式图

Pt₃N.南华系; Pt₃X.下江群; Pt₃F.梵净山群

Figure 4. Evolution model of the ancient oil reservoirs in Jinning period in Fanjingshan area

下载: 全尺寸图片幻灯片

表 1 沥青样品Re、Os同位素比值

Table 1. Re and Os isotope ratio of asphalt samples

样品号	Re w_B/10^-9	Os w_B/10^-12	¹⁸⁷Re w_B/10^-9	¹⁹²Os w_B/10^-12	¹⁸⁷Osr w_B/10^-12	¹⁸⁷Osr占比/%	¹⁸⁷Re/¹⁸⁸Os	¹⁸⁷Os/¹⁸⁸Os
BT1	368.7	4 170.3	231.8	142.7	3 821.3	99.8	5 139.3	84.9
BT2	495.2	6 422.0	311.2	139.2	6 081.6	99.9	7 075.6	138.5
BT3	160.7	1 372.9	101.0	116.4	1 088.2	99.3	2 746.4	29.8
BT4	1 231.2	13 034.4	773.9	252.1	12 417.8	99.9	9 714.0	156.1
BT5	780.2	6 921.2	490.4	257.8	6 290.9	99.7	6 021.1	77.4
BT7	890.5	8 979.7	559.7	228.1	8 421.8	99.8	7 764.9	117.0

下载: 导出CSV

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