鄂尔多斯盆地苏里格气田中奥陶统马家沟组五段凝块石类型与古盐度初步分析

doi:10.7605/gdlxb.2020.01.006

古地理学报 ›› 2020, Vol. 22 ›› Issue (1): 97-110. doi: 10.7605/gdlxb.2020.01.006

• 岩相古地理学及沉积学 • 上一篇下一篇

鄂尔多斯盆地苏里格气田中奥陶统马家沟组五段凝块石类型与古盐度初步分析

乔亚斌¹, 张林¹, 王予¹, 张一果¹, 马君霞², 姜红霞³

1 中国石油长庆油田分公司第五采气厂,内蒙古鄂尔多斯 017300;
2 北京大成恒泰科技有限公司,北京 100029;
3 河北地质大学古生物研究院,河北石家庄 050031

收稿日期:2019-07-13 出版日期:2020-02-01 发布日期:2020-03-04
通讯作者: 姜红霞,女,1976年生,助理研究员,古生物学与地层学专业硕士研究生导师,主要研究方向为微生物碳酸盐岩、古生态学与化学地层学。E-mail: jianghx@hgu.edu.cn。
作者简介:乔亚斌,男,1975年生,高级工程师,长庆油田分公司第五采气厂总地质师,从事气田开发技术管理工作。E-mail: qyb_cq@petroChina.com.cn。

Thrombolite types and seawater palaeosalinity of the 5^th Member of Middle Ordovician Majiagou Formation in Sulige Gas Field,Ordos Basin

Qiao Ya-Bin¹, Zhang Lin¹, Wang Yu¹, Zhang Yi-Guo¹, Ma Jun-Xia², Jiang Hong-Xia³

1 Gas Production Plant 5 of PetroChina Changqing Oilfield Company,Ordos,Inner Mongolia 017300,China;
2 Beijing Dacheng Hengtai Technology Co.,Ltd.,Beijing 100029,China;
3 Paleontology Institute,Hebei GEO University,Shijiazhuang 050031,China

Received:2019-07-13 Online:2020-02-01 Published:2020-03-04
Contact: Jiang Hong-Xia,born in 1976,research assistant,is a supervisor of master degree candidate of paleontology and stratigraphy. Her researches focus on carbonate paleontology,reefs and microbialites,paleoecology and chemostratigraphy. E-mail: jianghx@hgu.edu.cn.
About author:Qiao Ya-Bin,born in 1975,senior engineer of gas field development,chief geologist of Gas Production Plant 5 of PetroChina Changqing Oilfield Company. He works on gas field development technical management. E-mail: qyb_cq@petroChina.com.cn.

摘要/Abstract

摘要： 微生物碳酸盐岩是近年来地学界研究的一个热点,其时空分布非常广泛,并可形成重要的油气储集层。在鄂尔多斯盆地北部苏里格气田的中奥陶统马家沟组马五1+2段和马五4段,笔者分别发现了非钙化微生物成因的凝块石微生物岩。依据显微结构,将凝块石划分为蠕虫状凝块石、网状凝块石和房室孔洞状凝块石3种类型。通过与基里巴斯现代超盐湖微生物碳酸盐形成环境的对比,推测在华北地台云坪广布、坪中有湖的大背景下,凝块石是在相对海平面上升、盐度大约在60‰~149‰之间的条件下形成的,而含石膏结核碳酸盐岩是在相对海平面下降、盐度达到149‰以上的条件下形成的。进一步研究发现,蠕虫状凝块石泥粉晶白云岩的白云石晶间孔和溶蚀孔非常发育,网状凝块石和房室孔洞状凝块石的溶蚀残余孔较发育,推测凝块石微生物岩具有较好的物性,是未来油气勘探的重要目标岩性之一。

关键词: 凝块石, 微生物岩, 奥陶系, 马家沟组, 鄂尔多斯盆地

Abstract: Studied on well cores of the 5^th Member of Ordovician Majiagou Formation in the Ordos Basin,it reveals that the microbialites in the 2^nd layer of $Ma^{4}_{5}$,the 2^nd layer of $Ma^{2}_{5}$,the 4^th layer of $Ma^{1}_{5}$ can be divided into three distinct types: wormlike thrombolite,bacterial netlike thormbolite and chamber-patches thrombolite. By comparing with formation conditions of the modern microbial carbonate in the hypersaline lakes in the Republic of Kiribati,it is inferred that (1)the studied thrombolites formed in hypersaline lakes with salinity of 60‰~149‰ as the relative sea level rose,and(2) the gypsum-bearing carbonates formed in the hypersaline lakes with salinity of above 149‰. The wormlike thrombolites have high contents of intercrystaline pores and dissolution pores,and the netlike and chamber-patches thrombolites have high contents of relict pores, which makes thrombolites as an important exploration target.

Key words: thrombolite, microbialite, Ordovician, Majiagou Formation, Ordos Basin

中图分类号:

P588.24+8

乔亚斌, 张林, 王予, 张一果, 马君霞, 姜红霞. 鄂尔多斯盆地苏里格气田中奥陶统马家沟组五段凝块石类型与古盐度初步分析[J]. 古地理学报, 2020, 22(1): 97-110.

Qiao Ya-Bin, Zhang Lin, Wang Yu, Zhang Yi-Guo, Ma Jun-Xia, Jiang Hong-Xia. Thrombolite types and seawater palaeosalinity of the 5^th Member of Middle Ordovician Majiagou Formation in Sulige Gas Field,Ordos Basin[J]. JOPC, 2020, 22(1): 97-110.

http://www.gdlxb.cn/CN/Y2020/V22/I1/97

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鄂尔多斯盆地苏里格气田中奥陶统马家沟组五段凝块石类型与古盐度初步分析

Thrombolite types and seawater palaeosalinity of the 5^th Member of Middle Ordovician Majiagou Formation in Sulige Gas Field,Ordos Basin

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Thrombolite types and seawater palaeosalinity of the 5^th Member of Middle Ordovician Majiagou Formation in Sulige Gas Field,Ordos Basin