| 摘要：正 厚达1。5km 的 Phuket 群广泛分布于泰国半岛的南部，主要由一套冰海硅质碎屑岩序列组成，可与阿拉斯加及南极的第四纪冰海沉积序列相对比，也可与典型的冈瓦纳冰川沉积相对比。根据其中的Metalogoceras of involutum 确定 Phuket 群顶部的时代为亚丁斯克阶。从整个 Phuket 群中找到的腕足化石表明，其地质时代属于萨克马尔阶。在整合上覆的 Rat Buri 灰岩中发现了伦纳德阶的牙形石化石。在这套灰岩中也找到了亚丁斯克阶晚期至孔古尔阶的腕足类化石，泰语论文网站，泰语论文，这可以解释它与澳大利亚西部相近时代地层之间的关系。 Abstract：Is as thick as 1. 5km Phuket is widely distributed in southern Thailand Peninsula, is mainly composed of a set of glaciomarine siliciclastic sequence, compared with the Alaska and Antarctica in the Quaternary glacial marine sedimentary sequence, compared with typical Gondwana glacial deposits. According to the Metalogoceras of involutum Phuket group at the top of the Aden times Smolensk order. Find from the Phuket group of brachiopod fossils show that the geological age belongs to sakmarian. In the integration of the Buri Rat limestone, the Leonard order was found in the shape of the. In the limestone also found the Artinskian stage advanced to the hole Gul order of brachiopods fossils, which can explain it with Western Australia close relationship between the age of the strata. 引言：厚达1.5 km的Phuket群广泛分布于泰国半岛的南部,主要由一套冰海硅质碎屑岩序列组成,可与阿拉斯加及南极的第四纪冰海沉积序列相对比,也可与典型的冈瓦纳冰川沉积相对比。根据其中的万e‘。10,。ce,。。Cf‘二。。l:t。。确定Phuket群顶部的时代为亚丁斯克阶。从整个Phuket群 |
