西藏札达盆地上新统古格组和托林组的厘定与层序地层划分

Geological Bulletin of China(2007)

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Abstract
根据札达盆地剖面中地层的接触关系、沉积旋回、沉积体系和岩相岩性特征,可将上新统河湖相地层划分为2个组、5个沉积相、8个岩段.古格组(N22g)一岩段为砾岩,属河流相沉积;二、三、五岩段以细碎屑岩为主,属浅湖相沉积;四岩段以含粘土质细碎屑岩为主,属深湖相沉积.托林组(N21t)一、二、三岩段为一套砾岩、含砾中粗粒钙质长石岩屑砂岩和中细粒砂岩的碎屑岩,为典型冲(洪)积扇沉积物.ESR法和古地磁法测年结果表明,古格组形成时代为上新世晚期(4.40~2.47 Ma);托林组形成时代为上新世早期(5.44~4.40 Ma).札达盆地为一同生断陷盆地,在上新世时期的构造运动过程中,盆地演化经历了水进体系域-湖泊扩张体系域-湖泊收缩体系域3个发展阶段.
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Key words
Fluvio-lacustrine sediments,Guge and Toling formations,Pliocene,Sequence stratigraphy,Tibet,Zanda basin
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