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早奥陶世塔里木盆地继承了晚寒武世的海进过程，一直持续至中奥陶世晚期并达到顶峰。该时期塔里木盆地发育一个碳酸盐岩台地，其主体区以浅水碳酸盐沉积为主，但柯坪-塔中-古城一带存在一个相对深水的台坳，表现出与主体区不同的沉积特征。
塔里木盆地鹰山组生物潜穴白云岩成因机理
【摘 要】
：
早奥陶世塔里木盆地继承了晚寒武世的海进过程，一直持续至中奥陶世晚期并达到顶峰。该时期塔里木盆地发育一个碳酸盐岩台地，其主体区以浅水碳酸盐沉积为主，但柯坪-塔中-古城
【机 构】
：
中国科学院地质与地球物理研究所,北京100029;中国科学院大学研究生院,北京100049中国科学院地质与地球物理研究所,北京100029
【出 处】
：
2015全国沉积学大会
【发表日期】
：
2015年10期
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