【摘要】 <正> 石钱组滩系袁复礼教授(1938)建立的“石钱滩建造”演化而来.该组分布于克拉麦里山以南,沿准噶尔盆地东北缘呈北西、南东向展布.石钱滩组含无脊椎动物化石丰富,并有油气迹象,从而引起广大地质工作者的注意.1984、1985年笔者与新疆地矿局第二区调大队四分队合作,对石钱滩组进行了详细的野外工作,取得了丰富的化石和地层资料.在此基础上,本文试对石钱滩组的古气候特征作初步探讨,不足之处,请批评指正.更多还原

【Abstract】 The Shiqiantan Formation of late Carboniferous is distributed to the northeast margin of Junggar Basin, which is mainly composed of bioclastic limestone and mudstone with aboundant fossils.Based on palaeontology ( including bivalve, coral, siliceous sponge and palaeoflora ) , fossil fragment association, clay minerals, lith-ostratigraghy and oxygen isotope geothermometry.the palaeoclimatic characteristics of the Shiqiantan Formation has been discussed in this paper. The authors have come to a conclusion that the Shiqiantan Formation was formed in the semiarid and warm temperate climate. Some possible factors affecting the climate, such as palaeolatitude, atmospheric circulation, plate movement, are analysed.更多还原