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现代地质 ›› 2015, Vol. 29 ›› Issue (5): 1061-1072.

• 天然气水合物调查评价专辑 • 上一篇    下一篇

青海木里聚乎更天然气水合物潜在区中侏罗世岩相古地理特征

邵龙义1,杨致宇1,李永红2,商晓旭1,王伟超2,吕景高1,文怀军3   

  1. (1.中国矿业大学(北京) 地球科学与测绘工程学院,北京100083;2.青海煤炭地质一0五勘探队,青海 西宁810007;3.青海煤炭地质局,青海 西宁810001)
  • 出版日期:2015-10-29 发布日期:2015-12-24
  • 作者简介:邵龙义,男,教授,博士生导师,1964年出生,煤田地质及环境科学专业,主要从事环境地球化学及煤田地质学的教学与研究工作。Email:shaol@cumtb.edu.cn。
  • 基金资助:

    神华青海能源开发有限责任公司“青海省天峻县聚乎更煤矿区三露天天然气水合物调查评价”项目(SHQHNY201307001);中国地质调查局油气资源调查中心“我国非常规能源矿产 调查评价选区研究”子课题 (1212011220794)。

Lithofacies Palaeogeography of the Middle Jurassic in the Juhugeng Gas Hydrate Potential Area in Muli,Qinghai Province

SHAO Long-yi1, YANG Zhi-yu1, LI Yong-hong2, SHANG Xiao-xu1, WANG Wei-chao2, Lv Jing-gao1, WEN Huai-jun3   

  1. (1.School of Geosciences and Surveying Engineering, China University of Mining & Technology, Beijing 100083, China;2.Qinghai No.105 Coal Geological Exploration Team, Xining, Qinghai 810007,China;3.Qinghai Bureau of Coal Geology, Xining, Qinghai 810001,China)
  • Online:2015-10-29 Published:2015-12-24

摘要:

青海聚乎更矿区不仅赋存丰富的煤炭资源,同时也是全球陆域中纬度高海拔地区天然气水合物的首要发现地,同时也是我国非常规天然气(煤层气和页岩气)勘探开发的潜在热点地区,且天然气水合物勘探的层位主要为中侏罗世含煤岩系。通过对青海聚乎更矿区中侏罗世含煤地层野外露头、钻孔岩心、测井等资料整理分析的基础上,对研究区内中侏罗世含煤岩系沉积时期的沉积环境及古地理进行了分析。以定量和定性分析相结合的方法对研究区岩相古地理进行重建。以钻孔沉积相分析为基础,结合单因素分析多因素综合作图法及研究区目的层段沉积相断面图分析,最终恢复各段沉积期的岩相古地理格局。木里组下段岩性主要为细砾岩、含砾粗砂岩及粗砂岩等粗粒岩性,分析认为木里组下段主要发育辫状河沉积;木里组上段随着水体的不断加深,发育形成 了研究区主采的下1、下2煤层,该段主要以三角洲沉积为主,同时研究区西南区域发育滨浅湖沉积;江仓组上段沉积时期,水体进一步加深,成煤环境逐渐变差,发育形成多套薄煤层,以三角洲沉积为主,西南区域的滨浅湖沉积范围进一步扩大;江仓组上段是发现水合物的主要层段,其岩性主要以油页岩、暗色泥岩等为主,含有典型的湖泊沉积的瓣鳃类化石,为湖泊沉积。总体上,聚乎更矿区在中侏罗世经历了辫状河、三角洲平原、三角洲前缘、滨浅湖、半深湖-深湖的持续变深的演化过程。

关键词: 聚乎更矿区, 中侏罗世, 岩相古地理, 天然气水合物

Abstract:

The Juhugeng mining area in Qinghai Province is not only a major site for abundant coal resources, but also the primary discovery site of gas hydrate in high plateau of the mid-latitude worldwide. The gas hydrate exploration horizon is mainly in the Middle Jurassic coal-bearing series. In this paper, we studied the sedimentary environments and palaeogeography of the Middle Jurassic coal-bearing series in the Juhugeng mining area by analysis of data from borehole cores and logging curves. The lithofacies paleogeography of each lithological member was reconstructed by using combination of the quantitative and qualitative analysis methods, and the single borehole and cross section depositional section analyses. The Lower Member of the Muli Formation is mainly composed of fine conglomerates, pebbly sandstones, and coarse-grained sandstones, reflecting a braided river depositional environment. The Upper member of the Muli Formation consists of sandstones, siltstones, and two thick coal seams, and this member was formed mainly in the deltaic sedimentary environment, with the shore-shallow lake environment being locally developed in the southwestern part of the mining area. The Lower Member of the Jiangcang Formation is dominated by the fine-grained sandstones and mudstones, intercalated with several coarse-grained sandstone beds and thin coal seams, and this member was mainly deposited in the lower delta plain and delta front environments, with the shore-shallow lake environment developed in the southwestern part of the area. The Upper Member of the Jiangcang Formation, where the gas hydrates were frequently discovered, is dominated by a succession of oil shale and dark mudstone containing bivalve fossils, reflecting a deep to semi-deep lacustrine environment. During the Middle Jurassic the Juhgeng area has experienced an overall deepening process from the braided fluvial, deltaic plain, delta front and shore-shallow lake, to shallow to deep lake environments.

Key words: Juhugeng mining area, Middle Jurassic, lithofacies paleogeography, gas hydrate

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