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1.
The Distribution and Dynamics of CO_2 Concentration in the Karst Soil System in Substopic Region;
热带岩溶山区夏季土壤CO_2浓度的分布状况与变化规律
2.
Hydrological character of epikarst in Southwest China
我国西南岩溶区表层岩溶带的水文动态分析
3.
Varying regulation of epikarst developing intensity in southwest Hubei karst area
鄂西南岩溶地区表层岩溶带发育强度变化规律研究
4.
Structure Characteristics and Distribution Law in Epikarst Zone,Karst Area of Southwestern Hubei
鄂西南岩溶地区表层岩溶带结构特征及其分布规律
5.
Changes of Land Use in Lakeside Zone of Karst Lakes in Stone Forest
石林景区岩溶湖泊湖滨带土地利用变化研究
6.
At lava Hot Springs in Idaho, visitors may bathe in the thermal mineral waters.
在爱达荷的溶岩温泉,游客可在热矿泉水中洗澡。
7.
Super-heated rock from Earth's core is surging to the crust, melting ice built up over thousands of years.
极热的岩石从地心升起 溶化了千年的冰山
8.
Hydrogeochemical characteristic and genesis of hot karst groundwater under coal-bearing strata in the western Cizhou
磁西煤系下岩溶热水水文地球化学特征及成因
9.
Karst Development Law and Treatment Measures of Foundation in Datang Power Plant,Linzhou
大唐林州热电厂岩溶发育规律及地基处理方案
10.
Study on Physical and Chemical Properties and Corrosion of Surface Karst Springs on Vertical Limatic Zones;
垂直气候带表层岩溶泉水的理化性质与溶蚀作用研究
11.
The Geological Model of Hydrothermal Activity in Outcrop and the Characteristics of Carbonate Hydrothermal Karst of Lower Paleozoic in Tarim Basin
塔里木盆地下古生界碳酸盐岩热液岩溶的特征及地质模型
12.
Characteristics of petrology and thermodynamics of selective dissolution of plagioclase in volcanic reservoir rocks
火山岩储层斜长石选择性溶蚀的岩石学特征和热力学条件
13.
Analysis on hydro-chemical features and origin of the hot spring in karst geothermal field,east Liaocheng city
聊城市东部岩溶地热田地下热水水化学特征及成因分析
14.
large genus of showy epiphytic or lithophytic or terrestrial orchids of tropical and subtropical America.
热带和亚热带美洲附生岩生或陆生艳丽的一个兰花大属。
15.
tropical and subtropical Old World epiphytic or lithophytic ferns.
生长于热带和亚热带旧大陆的附生或岩生蕨类植物。
16.
epiphytic or lithophytic or terrestrial ferns of tropical Old World.
热带旧大陆的附生、岩生或陆生蕨类植物。
17.
venomous tropical marine fish resembling a piece of rock.
外表象一小块岩石的有毒的热带海生鱼。
18.
Similarly, high heat flows are to be expected among the active or not-too-long extinct magmatic belts of plate approximation zones.
同样,在板块相互靠近的地带的活动岩浆带或熄灭不久的岩浆带中也可以出现高热流。