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托索湖—花石峡礁带的主体由块状的礁相灰岩和生物碎屑灰岩所组成；
The reef island belt from Tusuo Lake to Huashixia is mainly composed of massive reef limestone and bioclastic limestone.
古城奥陶系礁滩相岩性圈闭带和罗布泊奥陶系礁滩相构造—岩性复合圈闭带。
Gucheng Ordovician reef beach facies lithostratigraphic trap zone and Luobupo Ordovician reef beach facies structure-lithostratigraphic trap zone.
过了许多许多年，地壳变迁，这一带海水退去，成了陆地，两个石礁就是现在的双塔山。
After a many, many years, the earth's crust changes, which bring water receded, became the land, two rock reef which is now Shuang Tashan.
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