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1·The reef island belt from Tusuo Lake to Huashixia is mainly composed of massive reef limestone and bioclastic limestone.

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；

2·This paper introduces the geological features and the unhomogeneous weathering phenomenon of coral reef limestone of Sudan Port Area, and the bearing capacity of this layer.

简单介绍苏丹港区珊瑚礁灰岩的地质特征及不均匀风化现象，以及该层的地基承载力。

3·Bleaching occurs when the tiny plant-like coral organisms die, often because of higher temperatures, and leave behind only a white limestone reef skeleton.

细小而形似植物的珊瑚生物死亡时会褪色变白，原因通常是不断升高的温度，留下的只是一具白色的石灰岩珊瑚礁骨架。

4·In return for a cozy, safe place to live, the algae provide the building blocks polps need to survive and make limestone to build the reef structures.

进而为了使珊瑚虫有一个舒适和安全的住所，海藻为珊瑚虫提供了能够存活的建筑模块，从而造成了石灰岩来构建成礁结构。

5·Bleaching occurs when the organisms that make up coral die and leave behind the white limestone skeleton of the reef.

白化现象即组成珊瑚的生物于死亡后所留下、如石灰石般的骨骼。