塔里木盆地志留-泥盆系克拉通盆地气候层序发育模式研究

Study on Development of Climate Sequence Model in Silurian-Devonian System of Tarim Basin

在对存在多个地层划分分区的塔里木盆地志留-泥盆系地层进行了岩性地层的和层序地层的对比和划分基础上。并且其中在划分层序地层时融入了可容空间变化因素的影响。对存在于塔里木盆地志留-泥盆系台盆区的气候转变进行了深入分析,总结了气候在可容空间变化中的作用和以气候为主控因素的层序发育模式,提出了"气候层序发育模式",并且分析了气候层序发育过程中气候对层序发育的控制过程。

On the basis of constrast and division of litholigical stratum and sequence stratigraphy of Silurian-Devonian System of Tarim Basin,in which there existed many stratum division districts,the influence of the element of the accommodation was combined in sequence stratum.A study was made on the change of the climate of the stable area of Silurian-Devonian System in Tarim Basin,the function of the climate of the change of the accommodation was summarized.The model of the development of sequence is also summarized.The model of the development of the climate sequence is put forward.The process of climate controlling the development of the climate sequence is analyzed.