内蒙古二连盆地白音查干凹陷热水沉积序列探讨

郭强; 李子颖; 秦明宽; 钟大康; 张放东; 贾翠; 邬军

内蒙古二连盆地白音查干凹陷热水沉积序列探讨

1.
核工业北京地质研究院北京 100029;
2.
中国石油大学(北京)地球科学学院北京 102249;
3.
中原油田勘探开发科学研究院河南濮阳 457001;
4.
中国石油吐哈油田公司鲁克沁采油厂新疆鄯善 838200

基金项目: 国家自然科学基金项目（批准号：41072104）资助

详细信息

中图分类号: P512.2

计量

文章访问数: 931
HTML全文浏览量: 10
PDF下载量: 650
被引次数: 0

Discussion of Hydrothermal Sedimentary Sequence in Baiyinchagan Sag of Erlian Basin, Inner Mongolia

1.
Beijing Research Institute of Uranium Geology, Beijing 100029;
2.
College of Geoscience, China University of Petroleum(Beijing), Beijing 102249;
3.
Research Institute of Exploration and Development, Zhongyuan Petroleum Exploration Bureau, Puyang, Henan 457001;
4.
Lukeqin Oil Production Plant, Tuha Oilfield Company, PetroChina, Shanshan, Xinjiang 838202

摘要

摘要: 近年来在内蒙古二连盆地白音查干凹陷下白垩统发现一套夹于深—半深湖相泥岩中，富含泥级钠长石、铁白云石、钠沸石、水镁铁石、重晶石等特殊矿物成分的热水沉积岩。该套岩石测井曲线上显示出异常高的自然伽马（G_R=700~1 100 API），为正常泥质岩自然伽马值的2~4倍，电阻率出现特高（2 000 Ω·m）—特低（0.2 Ω·m）的剧烈变化。根据热水沉积岩的岩石学特征，通过多口单井岩芯的详细解剖，结合相应的测井响应特征，可将腾格尔组—都红木组的热水沉积岩划分为四个旋回，每一旋回呈现低自然伽马值岩性段——尖峰状高自然伽马值岩性段特征，所对应的岩性序列可将热水沉积过程划分为三个阶段：初期为热液溢流期，主要在正常湖相泥岩中形成白云石及沸石纹层、条带或夹层，相应的岩石为低自然伽马的白云质沸石质泥岩；随后随着热液活动增强，出现喷流，使初期溢流形成的半固结白云石沸石纹层发生变形破碎，形成具有同生变形构造的白云质泥岩、白云石沸石内碎屑颗粒岩，测井曲线上仍然显示为低自然伽马特征；最后由于热液活动能量衰减，再次进入缓慢溢流阶段，形成高自然伽马泥质白云岩及部分白云质泥岩。
- 二连盆地 /
- 白音查干凹陷 /
- 早白垩世 /
- 热水沉积序列
Abstract: The lower Cretaceous hydrothermal sedimentary rocks had been found in Baiyinchagan sag of Inner Mongolia Erlian basin in recent years. The hydrothermal sedimentary rocks were rich in special minerals including clay sized albite, ankerite, natrolite, franquanite, barite, etc., and were only developed in semi-deep to deep lacustrine facies. The hydrothermal sedimentary rock can also be characterized by its log response with extremely high GR(GR=700~1 100 API), which is 2~4 times that of natural gamma value of normal argillaceous, and remarkably fluctuation in resistivity logging from as high as 2 000 Ω·m to 0.2 Ω·m. By the petrologic characteristics of the hydrothermal sedimentary rocks,the detailed analysis of single well core,combined with the corresponding logging response features, four hydrothermal actives can be recognized in Tenggeer-Douhongmu formation in the study area. One hydrothermal process will form a low natural gamma value lithologic section-the peak shape high natural gamma value cyclic deposition. A complete hydrothermal process consists of three stages: ①Early overflow process which precipitate low GR dolomitic or zeolitic fine grain rock with dolomite and zeolite laminae, zebra or interface layer. And ②Jet flow process with increasingly active hydrotherm. The laminae or interface layer of dolomite and zeolite will be deformed or even disrupted and result in dolomitic fine grain rock and clastic rock consisting of dolomitic or zeolitic intraclasts. After the energy of hydrotherm exhausted the hydrothermal activity will return back. ③Sluggish overflow stage and results in argillaceous dolomite rock and partial dolomitic mudstone with extremely high GR response.
- Erlian Basin /
- Baiyinchagan sag /
- Early Cretaceous /
- hydrothermal sedimentary sequence

HTML全文

参考文献(21)

[1]	Bostrom K, Rydell H, Joensuu O. Langbank: An exhalative sedimentary deposit[J]. Economic Geology and the Bulletin of the Society of Economic Geologists, 1979, 74(5): 1002-1011
[2]	周永章, 付伟, 杨志军, 等. 雅鲁藏布江缝合带及藏南地区硅质岩微组构特征及其地质意义[J]. 岩石学报, 2006, 22(3):742-750[Zhou Yongzhang, Fu Wei, Yang Zhijun, et al. Microfabrics of chert from Yarlung Zangbo Suture Zone and southern Tibet and its geological implications[J]. Acta Petrologica Sinica, 2006, 22(3): 742-750]
[3]	周永章, 付伟, 杨志军, 等. 藏南地区中生代硅质岩的地球化学特征及其成因意义[J]. 岩石学报, 2008, 24(3):600-608[Zhou Yongzhang, Fu Wei, Yang Zhijun, et al. Geochemical characteristics of Mesozoic chert from southern Tibet and its petrogenic implications[J]. Acta Petrologica Sinica, 2008, 24(3): 600-608]
[4]	Lonsdale P. Nontransform offsets of the Pacific-Cocos plate boundary and their traces on the rise flank[J]. GSA Bulletin, 1985, 96(3): 313-327
[5]	Grassle J F. Hydrothermal vent animals: Distribution and biology[J]. Science, 1985, 229(4715): 713-717
[6]	陈多福, 陈先沛, 陈光谦, 等. 热水沉积作用与成矿效应[J]. 地质地球化学, 1997, 4(4):7-12[Chen Duofu, Chen Xianpei, Chen Guangqian, et al. Hydrothermal sedimentation and mineralization effect[J]. Geology-Geochemistry, 1997, 4(4): 7-12]
[7]	薛春纪, 刘淑文, 冯永忠, 等. 南秦岭旬阳盆地下古生界热水沉积成矿地球化学[J]. 地质通报, 2005, 24(10/11):927-934[Xue Chunji, Liu Shuwen, Feng Yongzhong, et al. Geochemistry of hydrothermal sedimentary mineralization in the Lower Paleozoic of the Xunyang Basin, South Qinling, China[J]. Geological Bulletin of China, 2005, 24(10/11): 927-934]
[8]	方维萱, 张国伟, 胡瑞忠, 等. 陕西二台子铜金矿床钠长石碳酸(角砾)岩类型及形成构造背景分析[J]. 岩石学报, 2000, 16(3):392-400[Fang Weixuan, Zhang Guowei, Hu Ruizhong, et al. Analysis on tectonic background of formation and characteristics of albite carbonate brecciaite from Ertaizi Cu-Au deposits in the Qinling orogen[J]. Acta Petrologica Sinica, 2000, 16(3): 392-400]
[9]	彭润民, 翟裕生. 内蒙古狼山—渣尔泰山中元古代被动陆缘热水喷流成矿特征[J]. 地学前缘, 2004, 11(1):257-268[Peng Runmin, Zhai Yusheng. The characteristics of hydrothermal exhalative mineralization of the Langshan-Zhaertai belt, Inner Mongolia, China[J]. Earth Science Frontiers, 2004, 11(1): 257-268]
[10]	李江海, 冯军, 牛向龙, 等. 华北中元古带硫化物黑烟囱发现的初步报道[J]. 岩石学报, 2003, 19(1):167-168[Li Jianghai, Feng Jun, Niu Xianglong, et al. The preliminary report on the discovery of black smoker chimney within the Mesoproterozoic sulphide deposit of North China[J]. Acta Petrologica Sinica, 2003, 19(1): 167-168]
[11]	冯胜斌, 周洪瑞, 燕长海, 等. 东秦岭二郎坪群硅质岩热水沉积地球化学特征及其地质意义[J]. 沉积学报, 2007, 25(4):564-573[Feng Shengbin, Zhou Hongrui, Yan Changhai, et al. Geochemical characteristics of hydrothermal cherts of Erlangping Group in East Qinling and their geologic significance[J]. Acta Sedimentologica Sinica, 2007, 25(4): 564-573]
[12]	曾志刚, 秦蕴珊. 大洋钻探对海底热液活动研究的贡献[J]. 地球科学进展, 2003, 18(5):764-769[Zeng Zhigang, Qin Yunshan. Contribution of ocean drilling to the study of seafloor hydrothermal activity[J]. Advance in Earth Sciences, 2003, 18(5): 764-769]
[13]	Reyes A G, Massoth G, Ronde, et al. Hydrothermal mineralization in arc-type submarine volcanoes[J]. Geochimica et Cosmochimica Acta, 2006, 70(18): A528
[14]	郑荣才, 王成善, 朱利东, 等. 酒西盆地首例湖相"白烟型"喷流岩—热水沉积白云岩的发现及其意义[J]. 成都理工大学学报:自然科学版, 2003, 30(1):1-7[Zheng Rongcai, Wang Chengshan, Zhu Lidong, et al. Discovery of the first example of "white smoke type" of exhalative rock(hydrothermal sedimentary dolostone) in Jiuxi Basin and significance[J]. Journal of Chengdu University of Technology: Science & Technology Edition, 2003, 30(1): 1-7]
[15]	郑荣才, 文华国, 范铭涛, 等. 酒西盆地下沟组湖相白烟型喷流岩岩石学特征[J]. 岩石学报, 2006, 22(12):3028-3038[Zheng Rongcai, Wen Huaguo, Fan Mingtao, et al. Lithological characteristics of sublacustrine white smoke type exhalative rock of the Xiagou Formation in Jiuxi Basin[J]. Acta Petrologica Sinica, 2006, 22(12): 3028-3038]
[16]	郭强, 钟大康, 张放东, 等. 内蒙古二连盆地白音查干凹陷下白垩统湖相白云岩成因[J]. 古地理学报, 2012, 14 (1):59-68[Guo Qiang, Zhong Dakang, Zhang Fangdong, et al. Origin discussion of the Lower Cretaceous lacustrine dolomites in Baiyinchagan sag, Erlian Basin, Inner Mongolia[J]. Journal of Palaeogeography, 2012, 14 (1): 59-68]
[17]	谭成仟, 刘池阳, 赵军龙, 等. 鄂尔多斯盆地高自然伽马值异常特征及主控因素研究[J]. 石油地球物理勘探, 2007, 42 (1):50-56[Tan Chengqian, Liu Chiyang, Zhao Junlong, et al. Study on feature of high natural gamma anomaly and main controlling factors in Ordos Basin[J]. Oil Geophysical Prospecting, 2007, 42 (1): 50-56]
[18]	邱欣卫, 刘池阳, 李元昊, 等. 鄂尔多斯盆地延长组凝灰岩夹层展布特征及其地质意义[J]. 沉积学报, 2009, 27(6):1135-1146[Qiu Xinwei, Liu Chiyang, Li Yuanhao, et al. Distribution characteristics and geological significances of tuff interlayers in Yanchang Formation of Ordos Basin[J]. Acta Sedimentologica Sinica, 2009, 27(6): 1135-1146]
[19]	王宣龙, 李厚裕, 冯红霞. 利用声波和自然伽马能谱分析泥岩裂缝储层[J]. 测井技术, 1996, 20(6):432-440[Wang Xuanlong, Li Houyu, Feng Hongxia. Analysis of fracture-type shale reservoir using acoustic and natural gamma ray spectrometry logs[J]. Well Logging Technology, 1996, 20(6): 432-440]
[20]	赵凤民. 中国碳硅泥岩型铀矿地质工作回顾与发展对策[J]. 铀矿地质, 2009, 25(2):91-97[Zhao Fengmin. An review on geology study of carbonaceous-siliceous-pelitic rock type uranium deposit in China and the strategy for its development[J]. Uranium Geology, 2009, 25(2): 91-97]
[21]	方适宜, 李佑威, 范少云. 海底热水沉积铀矿研究——以鄂西北碱性火山岩型与硅灰岩型铀矿为例[J]. 大地构造与成矿学, 1992, 16(1):105-106[Fang Shiyi, Li Youwei, Fan Shaoyun. Studies of submarine hydrothermal-sedimentary Uranium deposits[J]. Geotectonica et Metallogenia, 1992, 16(1): 105-106]

[1]	朱志才, 翟庆国, 胡培远, 唐跃, 王海涛, 王伟, 吴昊, 黄智强. 拉萨—羌塘地体碰撞时限：来自班公湖—怒江缝合带中段多尼组沉积的约束 . 沉积学报, 2020, 38(4): 712-726. doi: 10.14027/j.issn.1000-0550.2019.081
[2]	陈治军, 王志伟, 张少清, 高怡文, 韩长春, 李科社. 二连盆地宝勒根陶海凹陷烃源岩生物标志化合物特征与油源对比 . 沉积学报, 2020, 38(2): 451-462. doi: 10.14027/j.issn.1000-0550.2019.034
[3]	余坤, 屈争辉, 琚宜文, 薛志文. 二连盆地胜利煤田含煤地层埋藏史及热史分析 . 沉积学报, 2018, 36(5): 903-913. doi: 10.14027/j.issn.1000-0550.2018.064
[4]	闫志明, 邵龙义, 王帅, David Large, 汪浩, 孙钦平. 早白垩世泥炭地净初级生产力及其控制因素——来自二连盆地吉尔嘎郎图凹陷6号煤的证据 . 沉积学报, 2016, 34(6): 1068-1076. doi: 10.14027/j.cnki.cjxb.2016.06.006
[5]	. 二连盆地巴音都兰凹陷下白垩统湖相云质岩成因研究 . 沉积学报, 2014, 32(3): 560-567.
[6]	. 白音查干凹陷桑合地区腾格尔组储层特征及主控因素分析 . 沉积学报, 2013, 31(2): 350-357.
[7]	王建强. 鄂尔多斯盆地西南部下白垩统宜君组砾岩砾组分析及其意义 . 沉积学报, 2011, 29(2): 226-234.
[8]	梁宏斌. 断陷湖盆缓坡带高位三角洲体系与油气成藏组合特征分析——以二连盆地吉尔嘎朗图凹陷为例 . 沉积学报, 2011, 29(4): 783-792.
[9]	景山. 辽西建昌盆地早白垩世义县组沉积环境分析及盆地演化初探 . 沉积学报, 2009, 27(4): 583-591.
[10]	张英利. 滦平盆地上白垩统九佛堂组中的熔积岩及地质意义 . 沉积学报, 2008, 26(1): 105-110.
[11]	. 吉林松江盆地早白垩世大拉子组沉积特征及演化 . 沉积学报, 2008, 26(1): 61-69.
[12]	岳信东. 二连盆地白音查干凹陷下白垩统腾格尔组沉积相 . 沉积学报, 2008, 26(4): 593-601.
[13]	李双应, 李任伟, 王道轩, 刘因, 岳书仓, 孟庆任, 金福全. 大别山北缘早白垩世黑石渡组沉积体系研究 . 沉积学报, 2004, 22(4): 566-572.
[14]	许书堂, 马维民, 王德仁, 靳广兴, 李继东, 杨玉娥. 二连盆地白音查干凹陷下白垩统层序地层研究 . 沉积学报, 2004, 22(4): 644-650.
[15]	张开均, 夏斌, 夏邦栋, 王冠民, 张孟群, 李永铁, 叶和飞. 冈底斯弧弧后早白垩世裂谷作用的沉积学证据 . 沉积学报, 2003, 21(1): 31-37,65.
[16]	李勇, 王成善, 伊海生, 石和, 林金辉, 朱利东, 李祥辉. 青藏高原中侏罗世—早白垩世羌塘复合型前陆盆地充填模式 . 沉积学报, 2001, 19(1): 20-27.
[17]	林玉祥, 郝石生, 祝玉衡, 平学聪. 二连盆地化探普查成效分析 . 沉积学报, 1997, 15(2): 220-225.
[18]	江德昕, 魏俊超. 内蒙古查干诺尔盐湖晚更新世至全新世孢粉植物群与古气候 . 沉积学报, 1997, 15(S1): 147-151.
[19]	吉利明. 甘肃民和盆地早白垩世孢粉植物群的古气候环境和地理分区位置 . 沉积学报, 1994, 12(2): 133-142.
[20]	姚金福, 朱莲芳. 酒西盆地石北地区晚侏罗—早白垩世沉积相研究 . 沉积学报, 1989, 7(4): 105-111.

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 931
HTML全文浏览量: 10
PDF下载量: 650
被引次数: 0

姓名
邮箱
手机号码
标题
留言内容
验证码

留言板

内蒙古二连盆地白音查干凹陷热水沉积序列探讨

计量

Discussion of Hydrothermal Sedimentary Sequence in Baiyinchagan Sag of Erlian Basin, Inner Mongolia

计量

目录

内蒙古二连盆地白音查干凹陷热水沉积序列探讨

1. 核工业北京地质研究院北京 100029;

2. 中国石油大学(北京)地球科学学院北京 102249;

3. 中原油田勘探开发科学研究院河南濮阳 457001;

4. 中国石油吐哈油田公司鲁克沁采油厂新疆鄯善 838200

English Abstract

Discussion of Hydrothermal Sedimentary Sequence in Baiyinchagan Sag of Erlian Basin, Inner Mongolia

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

内蒙古二连盆地白音查干凹陷热水沉积序列探讨

计量

出版历程

Discussion of Hydrothermal Sedimentary Sequence in Baiyinchagan Sag of Erlian Basin, Inner Mongolia

计量

出版历程

目录

内蒙古二连盆地白音查干凹陷热水沉积序列探讨

1. 核工业北京地质研究院 北京 100029; 2. 中国石油大学(北京)地球科学学院 北京 102249; 3. 中原油田勘探开发科学研究院 河南濮阳 457001; 4. 中国石油吐哈油田公司鲁克沁采油厂 新疆鄯善 838200

English Abstract

Discussion of Hydrothermal Sedimentary Sequence in Baiyinchagan Sag of Erlian Basin, Inner Mongolia

全文HTML

目录

友情链接

期刊在线

联系我们

1. 核工业北京地质研究院北京 100029;

2. 中国石油大学(北京)地球科学学院北京 102249;

3. 中原油田勘探开发科学研究院河南濮阳 457001;

4. 中国石油吐哈油田公司鲁克沁采油厂新疆鄯善 838200