2) burial dissolution
埋藏溶蚀作用
1.
Characteristics of burial dissolution in the Ordovician limestone of Tahe Oilfield;
塔河油田奥陶系灰岩埋藏溶蚀作用特征
2.
The comprehensive study of some samples from the Ordovician granule limestone in Tarim Basin showed that the burial dissolution could be classified as in-source dissolution and out-source dissolution based on the macro-microcosmic petrology and geochemistry features.
塔里木盆地奥陶系颗粒石灰岩的岩石学和地球化学综合研究表明,埋藏溶蚀作用可分为内源溶蚀和外源溶蚀两个作用阶段,这两种溶蚀作用的本质区别是酸性流体的来源和流体运移途径不同。
4) buried karstification
埋藏岩溶
1.
Based on lithology,geophysical data and test data,the authors divided karstification of northern Tarim Basin into three types(penecontemporaneous karstification,buried karstification,weathering karstification)and some subtypes.
本文以岩石学、地球物理资料及测试分析资料为基础,将塔北地区奥陶系碳酸盐岩古岩溶划分为准同生岩溶、埋藏岩溶、风化壳岩溶三大类及若干亚类。
5) deep-lying dissolution
深埋溶蚀
6) buried erosion surface
埋藏侵蚀面
补充资料：孤峰溶蚀平原
孤峰溶蚀平原是指峰林平原进一步发育，峰林不断溶蚀降低，地表夷平，仅有少量山峰存在所形成的平原
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条