The main copper mineral is atacamite on the surface, which form on droughty climate conditions in salt basin.
主要的地表铜矿物是氯铜矿,为干旱气候条件下含盐盆地的产物。
As they drilled into the central and deepest part of the Mediterranean basin, the scientists took solid, shiny, crystalline salt from the core barrel.
随着科学家们在地中海盆地的中部和最深处进行钻探,他们从岩心桶中取出了坚硬的、有光泽的结晶盐。
Known as' the world of salt ', Tsaidam Basin boasts three features: the greatest amount of reserves around the world plus a high quality and variety of salt.
誉满全球的“世界盐都”,柴达木盆地有以三种容貌而闻名:世界上最多数量的保护区加上高质量和多种类的盐。
Qaidam basin, located in the provincial Northwest, most of the Gobi Desert and over the eastern marshes, Salt Lake, the terrain is typical of the highest plateau inland basins.
柴达木盆地位于创省西北部,大部分为戈壁、沙漠,东部多沼泽、盐湖,是我国地势最高的典型的内陆高原盆。
The paper introduces the general situation of exploitation and utilization of salt lake mineral resources in the Chaidamu basin of Qinghai province.
文章介绍了青海省柴达木盆地盐湖矿产资源的概况、特点以及开发利用现状。
The model simulated the impact of engineering measures on the aquatic environment, water balance, water conversion, water & salt dynamics, and water consumption in the Basin.
模型较好地模拟各项工程措施对流域水环境、水平衡、水转换、水盐以及耗水等的影响。
Qarhan Salt lake is a typical closed lake in the dry Qaidam basin.
柴达木盆地的察尔汗盐湖是典型的干旱地区封闭湖泊。
Nonsandstone reservoirs between salt beds of Qianjiang Formation in the Qianjiang Sag of the Jianghan Basin are mainly composed of dolomicrite, glauberite rock, mudstone and their peperite.
组成江汉盆地潜江凹陷潜江组盐间段非砂岩储层的岩石主要为泥晶白云岩、钙芒硝岩、泥岩及其混积岩,孔渗性普遍较差。
The majority of salt-bearing basins in the world are petroliferous basin.
世界上大多数含盐盆地都是含油气区。
The salt deposits in Qarhan Basin are cited as a typical example of a modern dry salt lake.
察尔汉盆地是现代干盐湖的一个典型实例。
Wangbei block lies in northwest pitching end of the Wangchang salt swell in the Qianjiang depression, Jianghan basin and is characterized by typical salt lake deposit.
位于江汉盆地潜江凹陷王场盐隆背斜构造西北倾末端的王北区块具有典型的盐湖沉积。
There are rich mineral resources in the Qaidam Basin, such as the "four great treasures": salt, oil, lead zinc and borax.
盆地内部有丰富的矿产资源,人们称它为“聚宝盆”。盐、石油、铅锌和硼砂是盆地中的“四大宝”。
The salt-related tectonics in the Qiangtang basin mainly formed in late Jurassic and was further patterned during Cenozoic.
羌塘盆地盐相关构造形成于侏罗纪末并在新生代进一步定型。
On the basis of the existing information, the present article makes an approach to K-bearing property of the marine Triassic and search for potash salt in Sichuan basin.
据现有资料,阐述了四川盆地三叠系含钾性及找钾的现实意义。
Due to the extremely arid climate and high salt context in soil and underground water, the vegetation is very sparse and only 12 species of plants were found in the center of Tarim basin.
塔克拉玛干沙漠公路沿线气候恶劣、土壤和浅层地下水的含盐量高,沿线天然植被稀少,沙漠腹地仅发现12种能忍耐干旱和抗盐的植物种。
The rock types, climate patterns, lake basin and hydrological conditions in this region are contributory to the enrichment of trace elements in salt lake waters.
区域出露的岩性、气候、湖盆及水文等为盐湖水中富集痕量金属创造了有利条件。
Sequence stratigraphy study shows that Dongpu Sag is an inland salt lake basin with many nearby provenances and sedimentation centers.
通过高精度层序地层学的研究,认为东濮凹陷是一个多物源、近物源、具有多个沉积沉降中心的内陆盐湖盆地。
The studies indicate that the fluid formed during the basin mountain transition is metamorphic fluid with multi phase salt water formed in the initial stage of deformation.
盆山转换时期所形成的变质流体为多相盐水流体,形成于变形的初期。
From this it is concluded that we should search for liquid potash salt in Sichuan basin.
面对这一现实,理顺和拓宽四川找钾思路,勘查开发液态钾盐,是四川找钾的新方向。
Qianjiang Formation reservoir is the most important productive series in Jianghan Salt Lake Basin.
潜江组储层是江汉盐湖盆地最重要的产油层系。
Clay minerals are widely distributed in the salt-bearing series in the Arming basin.
粘土矿物在安宁盆地含盐系中分布很广。
Sedimentological methods have been applied to study the sedimentary facies and characteristics of the flourish stage of the development of the salt lake in this tectonic basin.
本文用沉积学方法探讨了该盆地渐新世早期常年盐湖沉积体系的沉积相特征、成盐方式、相带分布及控制因素。
Fold-thrust belts and salt-related structures are very prevalent in the Kuqa foreland fold-thrust belt of Tarim Basin in Northwest China.
褶皱-冲断带和盐相关构造均十分发育的秋立塔克地区构造极其复杂,该地区新生界内部存在两套起滑脱层作用的膏盐层。
Fold-thrust belts and salt-related structures are very prevalent in the Kuqa foreland fold-thrust belt of Tarim Basin in Northwest China.
褶皱-冲断带和盐相关构造均十分发育的秋立塔克地区构造极其复杂,该地区新生界内部存在两套起滑脱层作用的膏盐层。
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