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桂林地区中泥盆世吉维期牙形刺varcus带之下以滨岸碎屑岩沉积为主,varcus带开始记录碳酸盐岩沉积,持续到早石炭世;由生物礁和藻碳酸盐岩构成重要的岩性段.有关礁组合的一般沉积特征见1991年的野外参观手册.文中提到的研究点见图1.1 礁组合亚相类型、特征及发育桂林泥盆纪礁组合的沉积特征和生物特征与澳大利亚坎宁盆地的泥盆纪礁组合具有一
In the middle Devichian period of Guijia, Guilin, the variational belt was dominated by clastic rocks along the shoreline. The varcus belt started to record carbonate sediments and continued to the Early Carboniferous. The reef and algae carbonate Rocks make up an important lithological segment and the general sedimentary characteristics of the reef assemblages are described in the field visit manual of 1991. The study points mentioned in the article are shown in Figure 1.1 Reef assemblage subfacies, characteristics and sedimentary characteristics of the Devonian reef combination in Guilin And biological characteristics with the Devonian reef combination of the Canning Basin, Australia