1) distributing of karst
岩溶分布
1.
This paper presents plentiful data of geology and exploration,summarizes the distributing of karst in Wuhan,and makes the conclusion that there are a lot of karst in the low layer and hole of karst is small.
研究武汉市岩溶分布与发育规律,对于岩溶地面塌陷地质灾害防治、岩溶地区建(构)筑物基础设计与施工、岩溶地下水研究等有重要作用。
2) development and distribution of fossil karst
古岩溶发育与分布
3) karst stages
岩溶分期
4) palaeokarst zone
岩溶分带
5) paleokarst distribution
岩溶分区
1.
Based on paleohydrological geology, L11 reservoir paleokarstification and the influence of pale-ofluid chemistry and dissolution stage on the development of paleokarst are studied in detail,and then paleokarst distribution is also discussed.
应用古水文地质方法综合分析了L_1~1储层古岩溶发育特征,阐述了溶蚀期次对古岩溶发育程度的影响,并进行了岩溶分区。
6) solute distribution
溶质分布
1.
Microstructure and solute distribution of Fe-Cr-Si-B Cladding by plasma;
等离子体表面熔覆Fe-Cr-Si-B涂层的显微组织与溶质分布
2.
The formation of band-like microstructures is related to the solute distribution ahead of solid-liquid interface,and the changes of the growth rate and alloy.
从实验和理论两方面阐明了上述带状组织的产生与合金定向凝固界面前沿的溶质分布有关;形成的原因是合金未达到稳态凝固,凝固速率和合金成分一直处于变化之中。
3.
The solute distribution during nonequilibrium solidification process was measured by EPMA .
通过形态分析确定了Al Mg Si合金的凝固顺序 ,用EPMA测定了非平衡过程的溶质分布 ,并发现FeSiAl4～ 5相成分在高冷速时为FeSiAl5,而在低冷速时为FeSiAl4。
补充资料：岩溶地貌
即“喀斯特地貌”(461页)。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
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