马来西亚半岛二叠纪古地理

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摘要马来西亚半岛的二叠纪及晚古生代的岩石零星出露且分布成4个带,总体上与马来西亚半岛南北向走势一致。这4个带分布的范围不等,从各自不同的岩石序列来看,每个带的地质历史也有所区别。从西向东这4个带分述如下。带1:马来西亚北部—Langkawi,玻璃市和 Kedah西北部这个带的二叠系主要为中二叠统的 Chuping 灰岩,它与下伏的石炭系及下二叠统碎屑岩层序呈整合接触。这套地层以 Kedah 的 Kubang Pasu

作者 Chai Peng Lee 张振芳

机构地区 Department of Geology University of Malaya

出处《地质科学译丛》 1998年第4期61-61,共1页

关键词二叠纪古地理马来西亚半岛

分类号 P531 [天文地球—古生物学与地层学]

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地质科学译丛

1998年第4期

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