palaeokarst

palaeokarst

美 　英

• n.古岩溶；古喀斯特

英汉解释

n.	1. 古岩溶 2. 古喀斯特

例句

The well developed palaeokarst feature in it is due to multistage tectonic movement and its intrinsic sedimentary characteristics.

由于多期构造运动及沉积体系自身的特征使古岩溶十分发育。

So the research findings will provide reliable evidence for the palaeokarst reservoirs evaluation and favorable area optimization.

上述研究成果将为川东石炭系古岩溶型储层评价与有利区带优选提供可靠依据。

Many reverse faults develop in Ordovician palaeokarst in Tahe region, which include mainly NW, and NE, and EW, and SN directional.

塔河地区奥陶系发育加里东中期、加里东晚期—海西早期和海西晚期的逆断裂，断裂走向总体为NW向、NE向、EW向和SN向为主。

Hercynian palaeokarst slope and palaeokarst upland are favourable to the development of karst pores.

海西期古岩溶斜坡带和古岩溶高地是岩溶空隙发育的有利区。

The Ordovician palaeokarst had gone through 3 evolution stages and there are 7 types of developed patterns in the Huanghua Depression.

黄骅坳陷奥陶系古岩溶经历了3个演化阶段，具有7种发育模式。

Palaeokarst Characteristics and Controlling Factors of Marine Carbonate Rocks in Jianghan Plain and its Neighboring Areas

江汉平原及邻区海相碳酸盐岩的古岩溶特征及控制因素

Indication of Mineral Inclusion Characteristics to Palaeokarst Actions

矿物包裹体特征对古岩溶作用的指示性

Application of Seismic Physical Forward Modeling in Palaeokarst Reservoir Study

地震物理正演模拟在古岩溶储层研究中的应用

Restoration of Pre-Carboniferous Palaeokarst Landform in Central Ordos Basin

鄂尔多斯盆地中部前石炭纪岩溶古地貌恢复

Controlling Effects of Fault over Ordovician Palaeokarst in Tahe Region

塔河地区断裂对奥陶系古岩溶的控制作用

Palaeokarst development characteristics of Lower Paleozoic buried hill in Chengbei 30

埕北30下古生界潜山古岩溶发育特征