黄建国,马德胜,龙胜清.西藏塔惹增地区上白垩统竟柱山组的厘定及其意义[J].贵州地质,2014,31(3):206-209,240
西藏塔惹增地区上白垩统竟柱山组的厘定及其意义
Determination and Its Significance of Zhushan Formation, Upper Cretaceous in the Tarezeng area, Tibet
投稿时间:2013-04-01  
DOI:
中文关键词:  塔惹增  上白垩统  竟柱山组  厘定  西藏
英文关键词:Tarezeng  Upper Cretaceous  Jingzhushan formation  Determination
基金项目:
作者单位
黄建国 贵州省地质调查院,贵州 贵阳 550005 
马德胜 贵州省地质调查院,贵州 贵阳 550005 
龙胜清 贵州省地质调查院,贵州 贵阳 550005 
摘要点击次数: 1079
全文下载次数: 0
中文摘要:
      分布于塔惹增地区帕荣山一带的一套碎屑岩夹碳酸盐岩,对其时代归属缺乏可靠的古生物化石,一直颇有争议。前人根据岩性将其归为古近系日贡拉组,通过对此套地层详细的剖面研究表明其时代为上白垩统竟柱山组,其沉积环境为残留海相沉积,此套地层的时代厘定,为研究怒江洋在该地区的关闭提供了重要的基础地质资料。
英文摘要:
      In Parong mountain of Tarezeng area, lack of fossil which can ensure the date of clastic rock nip carbonate rock is controversial. According to the lithology, the former researcher thought it belongs to Rigongla formation of Paleogene System. By study the section detailed, it proved that this strata is Zhushan formation of upper Cretaceous, it sedimentary environment is relict sea facies sediment. The determination of this strata affords important geological information for the study of the close of Nujiang river.
查看全文  查看/发表评论  下载PDF阅读器