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川东地区华蓥山海相三叠系不同类型岩石对海水信息的保存性评估
  • ISSN号:1000-6524
  • 期刊名称:《岩石矿物学杂志》
  • 时间:0
  • 分类:P588.2[天文地球—岩石学;天文地球—地质学] P595[天文地球—地球化学;天文地球—地质学]
  • 作者机构:[1]成都理工大学油气藏地质及开发工程国家重点实验室,沉积地质研究院,四川成都610059
  • 相关基金:国家自然科学基金资助项目(40839908,40672072);教育部博士点基金资助项目(20050616005)
中文摘要:

通过对川东地区华蓥山海相三叠系不同岩石类型样品的微观组构、阴极发光和微量元素等分析表明:川东地区华蓥山海相三叠系不同的岩石类型样品具有不同的抵抗成岩蚀变能力,其对海水信息的保存程度也不一致;钙质泥岩所记录的有关信息已基本不能代表海水,多数微晶灰岩所记录的有关信息可以较好地代表海水,而粉晶白云岩只有部分样品可以代表海水的信息,同时传统上被认为更容易遭受成岩蚀变的颗粒灰岩反而出现低Mn、高Sr和弱阴极发光等特征,其可能与早期海水胶结作用或者深埋藏条件下封闭海源流体作用有关。

英文摘要:

Different types of marine carbonate rocks have different capabilities of resisting diagenetic alteration and preserving coeval seawater information.Aragonite and high-magnesium calcite minerals,for example,are liable to suffering from relatively strong diagenetic alteration,and their preservation of the coeval seawater information is therefore relatively poor;by contrast,low-magnesium calcite mineral has much better capability for preservation of the coeval seawater information.It is thus thought that the evaluation of marine samples of different rock types for their diagenetic alteration and preservation of the coeval seawater information is a necessary basic work in sedimentary geochemistry and chemostratigraphy.The analyses of rock fabrics,cathodoluminescence and trace elements of Triassic marine samples of different rock types from the Huaying Mountains of eastern Sichuan were conducted in this paper to evaluate their capabilities for resisting diagenetic alteration and preserving coeval seawater information.The results indicate that the calcareous mudstone samples show strong luminescence,their average Mn concentration is higher than 800×10-6,average Sr concentration is only 280×10-6,average Mn/Sr ratio is higher than 3.3,which is the highest average Mn/Sr ratio in all the samples of different rock types.The micrite samples mostly show extremely weak or weak luminescence,with only a few samples showing moderate or strong luminescence,their average Mn concentration is 213×10-6,average Sr concentration is 704×10-6,and average Mn/Sr ratio is 0.44.The very fine-crystalline dolomite shows relatively weak luminescence,their average Mn concentration is 119×10-6,average Sr concentration is 86×10-6,which is the lowest average Sr concentration in all the samples,and average Mn/Sr ratio is 1.46.The grainstone samples show no luminescence,their average Mn concentrations is only 4×10-6,which is the lowest average Mn concentration in all the samples,average Sr concentrations is 1 015×10-6,which is the highest aver

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期刊信息
  • 《岩石矿物学杂志》
  • 北大核心期刊(2011版)
  • 主管单位:中国科学技术协会 中国地质学会岩石学专业委员会
  • 主办单位:中国地质学会矿物学专业委员会 中国地质科学院地质研究所
  • 主编:侯增谦
  • 地址:北京市百万庄路26号地质所
  • 邮编:100037
  • 邮箱:yskwzazhi@sohu.com yskw@chinajournal.net.cn
  • 电话:010-68328475
  • 国际标准刊号:ISSN:1000-6524
  • 国内统一刊号:ISSN:11-1966/P
  • 邮发代号:82-52
  • 获奖情况:
  • 国内外数据库收录:
  • 美国化学文摘(网络版),美国地质文献预评数据库,美国剑桥科学文摘,日本日本科学技术振兴机构数据库,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:10602