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塔北隆起三叠系新近系的砂岩和粉砂岩中粘土矿物的分布特征及影响因素
  • ISSN号:0469-5097
  • 期刊名称:《南京大学学报:自然科学版》
  • 时间:0
  • 分类:TP181[自动化与计算机技术—控制科学与工程;自动化与计算机技术—控制理论与控制工程]
  • 作者机构:[1]南京大学地球科学与工程学院,南京210023, [2]新疆塔里木油田公司勘探开发研究院,库尔勒841000
  • 相关基金:国家自然科学基金(41172040,40772027)致谢叶宇达、苏贵珍和张光辉等在样品测试和样品制备方面给予了帮助;在样品采集方面得到了中国石油塔里木油田公司的杨海军总工的热心相助,在此一并表示感谢!
中文摘要:

利用 X射线衍射和电子探针实验方法来研究塔北隆起三叠系新近系的砂岩和粉砂岩中粘土矿物的分布特征及绿泥石的成分,获得了以下认识:(1)研究区存在三种粘土矿物组合类型:R0 I/S+I+Chl、Ka+Chl+I、I+Chl.绿泥石多型为Ⅱb型,根据绿泥石成分分为辉绿泥石和铁镁绿泥石.(2)研究区粘土矿物的纵向分布及绿泥石成分的变化与成岩作用的关系不是非常密切.利用岩石地球化学方法,结合区域地质构造演变史,获得影响本区粘土矿物组合纵向分布特征的主要因素是构造地质环境、沉积物源和古环境.研究结果显示,当层位处在构造活动强烈,物源区未经历强烈风化,沉积物为快速堆积,古气候为半干旱至干旱的环境时,形成的粘土矿物组合主要为R0 I/S+I+Chl;当层位处在构造地质环境稳定,物源区强烈风化,沉积物经历了一定的搬运后再沉积,并为湿润的古气候时,形成的粘土矿物组合主要为Ka+Chl+I.

英文摘要:

The research on clay minerals is an important way to solve some fundamental geological problems since it can sensitively reflect the geochemical environment of basin sediments and diagenesis.The formation,transformation and disappearance of clay minerals are complex geological processes these are controlled by many kinds of geological factors.For the continental sedimentary basins,the distribution of the clay minerals is the result of the interaction among the ancient environment,the diagenesis,the sources of the sediments,and etc.However,some of the factors have more influence on the distribution of the clay minerals than the others.All the factors that affected the distribution of clay minerals are related to the tectonic setting of the sedimentary basins and tectonic developmentnbsp;history.Tectonic movement is the most important controller to the sedimentation.The distribution of clay minerals is acting as an important record in response to these factors.The purpose of this paper is to investigate the characteristics of the clay mineral assemblages in different depths and different strata of Tabei Uplift,and to explore the main factors affecting the distribution of clay minerals in this area.The analysis has been done on the following two aspects:1 .By using X-ray diffraction and electron microprobe methods to study the distribution characteristics of the clay minerals and chlorite composition in the sandstone and siltstone of Tabei uplift from Triassic to Neogene, the following understandings have been obtained.(1)There are three types of clay mineral assemblages in the studied area:R0 I/S+I+Chl,Ka+Chl+I,and I+Chl.The chlorites belong to typeⅡb.According to the chlorite components,they can be defined as diabantite and brunsvigite.(2)The vertical distribution of the clay minerals and the variances in chlorite compositions in the area are not very closely related to their diagenesis.2.By using the rock geochemical method along with regional geological tectonic evolution history,it is re

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期刊信息
  • 《南京大学学报:自然科学版》
  • 中国科技核心期刊
  • 主管单位:中华人民共和国教育部
  • 主办单位:南京大学
  • 主编:龚昌德
  • 地址:南京汉口路22号南京大学(自然科学版)编辑部
  • 邮编:210093
  • 邮箱:xbnse@netra.nju.edu.cn
  • 电话:025-83592704
  • 国际标准刊号:ISSN:0469-5097
  • 国内统一刊号:ISSN:32-1169/N
  • 邮发代号:28-25
  • 获奖情况:
  • 中国自然科学核心期刊,中国期刊方阵“双效”期刊
  • 国内外数据库收录:
  • 美国化学文摘(网络版),美国数学评论(网络版),德国数学文摘,中国中国科技核心期刊,中国北大核心期刊(2004版),中国北大核心期刊(2008版),中国北大核心期刊(2011版),中国北大核心期刊(2014版),中国北大核心期刊(2000版)
  • 被引量:9316