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1)  Sanhu depression
三湖拗陷
1.
Oil geologic feature in Sanhu depression of Qaidam Basin and next exploration and study direction
柴达木盆地三湖拗陷石油地质特征及下步勘探与研究方向
2)  down-warped lacustrine basin
拗陷湖盆
1.
Sediment accumulation on the steep slope zone of the continental down-warped lacustrine basin and dynamics of sequence filling: An example from the Triassic Yanchang Formation in the Ordos Basin,eastern Gansu;
陆相拗陷湖盆陡坡带物质聚集及层序充填动力学特征——以鄂尔多斯盆地陇东地区三叠系延长组为例
3)  deep-water lacustrine basin
拗陷深水湖盆
4)  depression [英][dɪ'preʃn]  [美][dɪ'prɛʃən]
拗陷
1.
Inversion structure and structural evolution in Zhoukou depression;
周口拗陷的反转构造与构造演化
2.
Discussion on Tectonic Movement Process of Huanghua Depression;
黄骅拗陷构造运动程式探讨
3.
The research results show that the second order tectonic systems in the Basin control the oil generating depression and the zone of oil and gas enrichment, and the third or fourth order shear tectonic systems the oil and gas fields.
塔里木盆地是多构造体系复合的大型含油气区,盆内二级构造体系控制生油拗陷和油气富集带三、四级扭动构造控制油气田。
5)  Sanhu Depression
三湖坳陷
1.
Sequence stratigraphy of Quaternary Seven Spring Group of the Sanhu depression and prediction for prospective targets for hydrocarbons;
三湖坳陷第四系七个泉组层序地层及有利目标预测
2.
The Pliocence—Quaternary System self-source and self-reservoir natural gas reservoir of the Sanhu Depression lie in the east Qaidam Basin that has become one of the biggest four natural gas producing districts.
柴达木盆地东部三湖坳陷上新统—第四系自生自储的天然气藏,已成为我国四大天然气产区之一。
6)  Sanhu depression
三湖凹陷
1.
There is the commercial exploration perspective of lithologic biogas pool in the Sanhu depression of the Chaidamu basin, NW, China.
三湖凹陷为北陡南缓,北斜坡由于凹陷急剧沉降与边缘相对抬升形成多个挠曲褶皱带,坳陷内可形成2大类岩性生物气藏,即陡坡带岩性气藏和缓坡带岩性气藏。
补充资料:湖盆
湖盆
lake basin
    地表上汇集水体的相对封闭的洼地。形似盆状。湖盆成因有地壳运动形成的,如断陷湖盆、坳陷湖盆;还有外力作用形成的,如冰蚀湖盆、堆积湖盆等,此外也有人类经济活动形成的,如水库库区等。湖盆可以由5部分组成:湖岸、沿岸带、岸边浅滩、水下斜坡、湖盆底。湖泊面积的大小,湖盆地质条件和水流动态不同,湖盆的形态也有差异。研究湖盆的形态及其变化,有助于了解湖泊的起源、发展;湖泊的容积、湖水的理化性质和水文形势的变化。
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