鲁西南YZK-3钻孔的盐类矿物和锶同位素组成及其地质意义<sup>*</sup>

doi:10.7605/gdlxb.2026.022

古地理学报 ›› 2026, Vol. 28 ›› Issue (1): 278-289. doi: 10.7605/gdlxb.2026.022

• 岩相古地理学及沉积学 • 上一篇下一篇

鲁西南YZK-3钻孔的盐类矿物和锶同位素组成及其地质意义^*

李兆强¹(), 李明慧², 宋香锁³^,⁴^,⁵, 高黎明⁶, 唐璐璐³^,⁴^,⁵, 刘凤臣³^,⁴^,⁵, 杨斌³^,⁴^,⁵(), 余武生², 路淑毅⁷, 张译文²

1 山东省肥城市自然资源和规划局,山东肥城 271600
2 中国科学院青藏高原研究所,北京 100101
3 山东省地质科学研究院,山东济南 250013
4 国土资源部金矿成矿过程与资源利用重点实验室,山东济南 250013
5 山东省金属矿产成矿地质过程与综合利用重点实验室,山东济南 250013
6 山东省曹县自然资源和规划局,山东曹县 274400
7 河南省地震局,河南郑州 450018

收稿日期:2025-04-10 修回日期:2025-05-04 出版日期:2026-02-01 发布日期:2026-02-09
通讯作者: 杨斌,男,1975年生,研究员,研究方向为地质勘查找矿。E-mail: yangbin71311@163.com。
作者简介:
李兆强,男,1972年生,高级工程师,研究方向为地质勘查找矿。E-mail: gtjlzq@126.com。

Evaporates and strontium isotopes of borehole YZK-3 in southwest Shandong Province and their geological implications

LI Zhaoqiang¹(), LI Minghui², SONG Xiangsuo³^,⁴^,⁵, GAO Liming⁶, TANG Lulu³^,⁴^,⁵, LIU Fengchen³^,⁴^,⁵, YANG Bin³^,⁴^,⁵(), YU Wusheng², LU Shuyi⁷, Zhang Yiwen²

1 Feicheng Natural Resources and Planning Bureau of Shandong Province, Shandong Feicheng 271600,China
2 Institute of Tibetan Plateau,Chinese Academy of Sciences,Beijing 100101, China
3 Shandong Institute of Geological Sciences,Jinan 250013,China
4 Key Laboratory of Gold Mineralization Processes and Resource Utilization,Ministry of land and Resources,Jinan 250013,China
5 Key Laboratory of Metallogenic Geological Process and Resources Utilization in Shandong Province,Jinan 250013,China
6 Cao County Natural Resources and Planning Bureau of Shandong Province,Shandong Caoxian 274400,China
7 Henan Earthquake Agency,Zhengzhou 450018,China

Received:2025-04-10 Revised:2025-05-04 Online:2026-02-01 Published:2026-02-09
Contact: YANG Bin,born in 1975, researcher, is mainly engaged in research on geological survey and prospecting. E-mail: yangbin71311@163.com.
About author:
LI Zhaoqiang,born in 1972, senior engineer, is mainly engaged in research on geological survey and prospecting. E-mail: gtjlzq@126.com.

摘要/Abstract

摘要：

鲁西南黄岗潜凹陷发现了盐储量达到百亿吨级的古近纪盐类矿床,该矿床是中国东部罕见的超大型岩盐矿,深入研究该矿床成因对丰富中国的盐类矿床理论具有重要意义。本文选取YZK-3钻孔中519.9 m的含盐沉积物,从成因矿物学的角度,详细分析了矿物成因、成盐环境和成矿物质来源。盐类矿物中,碳酸盐矿物以方解石、白云石、铁白云石为主,文石少量; 硫酸盐矿物主要是硬石膏,少量石膏和天青石; 氯化物矿物只出现石盐一种矿物。根据这些矿物的分布特征和成因判断,始新世中晚期—渐新世时期古湖泊的演化过程为: 淡水湖—咸水湖—盐湖—咸水湖—淡水湖。石盐和硬石膏的⁸⁷Sr/⁸⁶Sr值为0.711227~0.71177,远高于同时代海水的。结合热液研究成果综合判断,黄岗潜凹陷成盐卤水中没有发现海相信息。除了岩石风化外,受大气降水影响的深部热液也是不可忽视的成盐物质来源。

关键词: 石盐, 石膏, 硬石膏, 锶同位素, 古近系, 黄岗潜凹陷

Abstract:

A massive Tertiary salt deposit containing 10 billion tons has been identified in the Huanggang buried sag of southwestern Shandong Province. This deposit is a rare super-large rock salt deposit in eastern China. To investigate the material sources and depositional environment of this salt formation,we conducted a comprehensive analysis of salt mineral assemblages,stratigraphic distributions,and 87Sr/86Sr isotopic compositions in halite and anhydrite from a 520-meter core(Borehole YZK-3)situated at the basin margin. Among the salt minerals,carbonate minerals mainly contained calcite,dolomite,ankerite and minor aragonite. Sulfate minerals contained anhydrite,with minor gypsum and celestite. Chloride minerals were composed of only halite. Based on their distribution and genesis,the paleolake evolution during the Middle-Late Eocene to Oligocene progressed through five distinct stages: freshwater→brackish→saline→brackish→freshwater lake systems. The⁸⁷Sr/⁸⁶Sr ratios measured in halite and anhydrite(0.711227-0.71177)significantly exceed contemporaneous seawater values. This isotopic disparity,combined with existing hydrothermal research data,demonstrates the absence of marine influences in the brine system.Substantial contributions from deep hydrothermal fluids mixed with meteoric waters was an important source of salt material.

Key words: halite, gypsum, anhydrite, strontium isotope, Paleogene, Huanggang buried sag

中图分类号:

P612

李兆强, 李明慧, 宋香锁, 高黎明, 唐璐璐, 刘凤臣, 杨斌, 余武生, 路淑毅, 张译文. 鲁西南YZK-3钻孔的盐类矿物和锶同位素组成及其地质意义^*[J]. 古地理学报, 2026, 28(1): 278-289.

LI Zhaoqiang, LI Minghui, SONG Xiangsuo, GAO Liming, TANG Lulu, LIU Fengchen, YANG Bin, YU Wusheng, LU Shuyi, Zhang Yiwen. Evaporates and strontium isotopes of borehole YZK-3 in southwest Shandong Province and their geological implications[J]. Journal of Palaeogeography（Chinese Edition）, 2026, 28(1): 278-289.

http://www.gdlxb.cn/CN/Y2026/V28/I1/278

图/表 6

图 1 鲁西南黄岗潜凹陷YZK-3钻孔位置

Fig.1 Borehole YZK-3 location in Huanggang buried sag in southwest Shandong Province

图 2 鲁西南YZK-3钻孔含盐层位的岩性、盐类矿物含量及沉积环境

Fig.2 Lithology,mineral content and sedimentary environment of halite bearing intevals in borehole YZK-3 in southwest Shandong Province

图 3 鲁西南YZK-3钻孔样品XRD图谱

Fig.3 X-ray diffraction patterns of sample from borehole YZK-3 in southwest Shandong Province

表 1 鲁西南YZK-3钻孔石盐与石膏的⁸⁷Sr/⁸⁶Sr值

Table 1 ⁸⁷Sr/⁸⁶Sr ratios of halite and gypsum from borehole YZK-3 in southwest Shandong Province

样品号	深度/m	矿物	⁸⁷Sr/⁸⁶Sr
YZK3-326.25	961.63	石盐	0.711 307
YZK3-327.50	962.88	石盐	0.711 482
YZK3-328.50	963.88	石盐	0.711 227
YZK3-328.60	963.98	石盐	0.711 262
YZK3-329.50	964.88	石盐	0.711 280
YZK3-334.25	969.63	石膏	0.711 534
YZK3-334.60	969.98	石膏	0.711 770

图 4 鲁西南YZK-3钻孔石盐和硬石膏的锶同位素及其与同时代海水及其他区域的对比

Fig.4 Comparison of Sr isotopes of halite and anhydrite from borehole YZK-3 in southwest Shandong Province with contemporaneous seawater and other areas

图 5 鲁西南YZK-3钻孔孔隙水^①与其他地区氢氧同位素的对比

Fig.5 Comparison of δ¹⁸O and δD of pore-water from borehole YZK-3 in southwest Shandong Province with those of other areas

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鲁西南YZK-3钻孔的盐类矿物和锶同位素组成及其地质意义^*

Evaporates and strontium isotopes of borehole YZK-3 in southwest Shandong Province and their geological implications

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鲁西南YZK-3钻孔的盐类矿物和锶同位素组成及其地质意义*

Evaporates and strontium isotopes of borehole YZK-3 in southwest Shandong Province and their geological implications

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鲁西南YZK-3钻孔的盐类矿物和锶同位素组成及其地质意义^*