李越,黄智斌,王建坡,王志浩,薛耀松,张俊明,张元动,樊隽轩,张园园

• 1:中国科学院南京地质古生物研究所
• 2:塔里木油田分公司勘探开发研究院

摘要(Abstract)：

塔里木盆地中央隆起区的中—上奥陶统灰岩相地层露头分布在巴楚良里塔格地区的一间房—唐王城。以牙形刺动物群为依据厘定3个组的时代,从下至上为一间房组(Periodus flabellum层、Pygodus serra层,属达瑞威尔阶)、吐木休克组(Pygodus anserinus层、Baltoniodus alobatus带,属桑比阶)和良里塔格组(含B.confluens动物群层,属凯迪阶下部)。一间房组的开始标志了新一期的海进,此组下段发育1期藻丘,中段发育1期藻丘、1期瓶筐石礁丘和3—4期瓶筐石—棘屑滩,上段代表了海水加深至浪基面之下的过程;吐木休克组沉积过程中达到了海进最大值,为凝缩沉积;良里塔格组代表了逐渐海退的过程,由浅滩和3期藻丘建造组成。

关键词(KeyWords)： 牙形刺;生物地层;沉积环境;一间房组;吐木休克组;良里塔格组;中—上奥陶统;巴楚;新疆

Abstract:

Keywords:

基金项目(Foundation): 中国科学院创新工程方向性项目(KZCXZ-YW-122,KZCX2-YW-Q05-01);; 国家自然科学基金项目(No.40572069,40532009);; 科技部973课题(2006CB806402);; 中石油塔里木油田分公司专项研究课题资助

作者(Author): 李越,黄智斌,王建坡,王志浩,薛耀松,张俊明,张元动,樊隽轩,张园园

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