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西藏当雄县九子拉地区侏罗纪盆地演化特征浅析
Analyses on Evolution Characteristics of Jurassic Basin in Jiuzila Area of Dangxiong,Tibet
【摘要】 处于班公湖—怒江—晶宁—孟连对接带南侧的九子拉区域,中-晚侏罗世,受北侧班公湖-怒江洋向南的持续俯冲,雅鲁藏布江弧后洋盆于早-中侏罗世向北低角度俯冲,在两者双向俯冲消减作用下,沿狮泉河-纳木错-嘉黎一线撕裂,造成该区弧后扩张,其间盆地经历了裂陷期→坳陷早期→主坳陷期→坳陷晚期沉积充填序列的演化过程,该区是冈底斯侏罗纪沉积盆地物质保存最完整的地区,对研究中生代冈底斯地质演化史分析具有较大意义。
【Abstract】 In the Jiuzala area of south Bangonghu-Nujiang-Jingning-Menglian junction belt,Middle-late Jurassic experienced continued south direction subduction of north Bangonghu-Nujiangyang and low angle north subduction of Yarlung Zangbu back-arc basin. Under the subduction of two direction,Shiquanhe-Namucuo-Jiali belt laniated and caused the back-arc expanded in this area,the basin experienced the evolution process of chasmic stage-early depression period-main depression period-late depression period sedimentary sequence. This area is the most perfect area where Gangdise Jurassic basin material kept.
【Key words】 Bangonghu-Nujiangyang; Jiuzila area; Back-arc expansion; Sedimentary basin; Jurassic; Tibet;
- 【文献出处】 贵州地质 ,Guizhou Geology , 编辑部邮箱 ,2015年03期
- 【分类号】P534.52
- 【被引频次】3
- 【下载频次】42