1) palaeokarst landform
古岩溶地貌
1.
The palaeokarst landform in west Lungu region was restored by using seismic horizon flattening technique.
以塔里木盆地轮古西地区为例,通过地震层拉平技术恢复了该区的古岩溶地貌,发现研究区岩溶地貌起伏变化很大,自东向西依次发育峰丛洼地、峰林谷地和峰林平原地貌组合。
2.
Through the sign recognition and the causes analysis of karstification,palaeokarst landform in the Huanglong Formation of Carboniferous is resumed with the erosion thicknesses method,geomorphologic method and impression method in eastern of the Sichuan Basin.
通过古岩溶作用标志识别和成因分析,采用残余地层厚度法、地貌法和印模法等技术手段对川东地区黄龙组古岩溶地貌进行恢复,从中划分出岩溶高地、岩溶斜坡和岩溶盆地三个岩溶地貌单元和峰丛、溶沟、落水洞、坡地、谷地、浅洼、残丘和槽地等微地貌单元,在平面上细分出七个典型的古岩溶地貌分区,并对分区内的岩溶地貌特征进行了研究,认为不同古岩溶地貌分区所处的地理位置及微地貌单元组成特征具有明显差异,从而直接影响到天然气藏的发育。
2) karstic palaeogeomorphology
岩溶古地貌
3) paleokarst landform gas reservoir
岩溶古地貌气藏
4) karst topography
岩溶地貌
1.
Xu Xia ke made a tour round thc North Mountains along Jinhua as a prclude to his system atlc research on karst topography.
徐霞客考察金华北山是他系统研究岩溶地貌的序幕。
5) karst landforms
岩溶地貌
1.
The karst landforms are very growth, and more than ten kinds of landform is formed.
平果岩溶堆积铝土矿是具有独特地质特征的铝土矿床 ,区内岩溶地貌十分发育 ,并且形成了多种地貌类型 ,本文主要探讨各类地貌特征 ,研究其发展和演化的规律 ,分析和论述地貌与成矿的关系 ,为该类型矿床地质工作提供参考。
2.
It is believed that the current limestone karst landforms on the plateau was originated from the Tertiary underground karst.
本文在野外考察的基础上并参照洞穴次生方解石的年代资料和有关文献 ,指出青藏高原目前所见到的岩溶地貌主要是第三纪古岩溶地下部分经后期剥蚀形成的。
6) karst landform
岩溶地貌
1.
The karst landform tailings dam disaster appraisal and the safe monitor are important for reducing the risk and the accident.
影响岩溶地貌某尾矿坝坝体稳定问题最突出的因素是:北西向、北东向构造的"棋盘格式";岩体整体性差、节理化;岩溶、洞隙、地表―地下"阶梯"水流运动模式;洪水和地震影响。
2.
A systematic comparison is made between the tourism scenery of Danxia landform and that of Karst landform by introducing their similarity and diversity in development condition,spatial distribution,physical scenery,and human scenery.
对丹霞地貌与岩溶地貌的旅游景观进行系统比较,揭示两者在发育条件及分布特点、自然及人文旅游景观方面的相似性与差异性。
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。
参考词条