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 组砂岩 The Permian and late Paleozoic rocks in Peninsular Malaysia are sporadically scattered and distributed in 4 zones, which is generally consistent with the trend of north and south of the peninsular Malaysia. The range of distribution of the four bands varies from different rock sequences, the geological history of each band is also different. The four bands from west to east are described below. Belt 1: The Permian in the northwestern part of Malaysia, Langkawi, Perlis and northwestern Kedah is mainly the Permian Chuping Limestone, which is integrated with underlying Carboniferous and Lower Permian clastic sequence . This formation is based on Kubang Pasu sandstone in Kedah