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1)  Baihu depression in Nanning basin
南宁盆地北湖坳陷
2)  depression Lake Basin
坳陷湖盆
1.
Topographic ramp often come into being in the edge of depression lake basin in the process of basin basement deformation under extrusion stress, the key factors controlling sequence development such as subsiding rate of basement and initial topographic slope have apparent difference on the two sides of ramp, which in.
坳陷湖盆在基底受压变形过程中 ,常在盆缘形成地形坡折带 ,以坡折为界 ,基底的沉降速率和原始地形坡度等控制层序发育的重要因素在其两侧均存在显著的差异 ,这在很大程度上控制了层序的发育模式和沉积体系的空间配置关系。
2.
The paper chose J1s-K1q1 formation in Shinan area, central Jungar basin asresearch object, which was typical gentle slope of depression lake basin andconducted sequence stratigraphic research, depositional facies research and oil poolforming rules research.
本文以准噶尔盆地腹部石南地区侏罗系三工河组~白垩系清水河组一段为研究对象,进行层序地层学、沉积学及油气成藏规律的综合研究,旨在明确坳陷湖盆缓坡层序及其主控因素的特点、沉积体系的时空演化规律以及岩性地层油气藏的分布规律,并以此指导岩性地层圈闭勘探的有利区带预测。
3)  downwarped lake basin
坳陷湖盆
1.
Significance of slope break zones in downwarped lake basins to exploration of non-structural traps in Junggar basin;
准噶尔盆地坳陷湖盆坡折带在非构造圈闭勘探中的应用
2.
Characteristics of slope breaks and their control on atectonic traps in downwarped lake basin;
坳陷湖盆坡折带特征及其对非构造圈闭的控制
4)  depression basin
坳陷盆地
1.
The Jurassic rocks in Qimugen-Sangzhuhe comprise Xilibili-Kuslapu fault basin and Damusi-Momoli- Keliyang depression basin separated by Qongkuoruolek anticline.
齐姆根—桑株河地区侏罗纪形成昔力必里-库斯拉甫断陷盆地和达木斯-莫莫克-克里阳坳陷盆地,其间以琼阔若勒克背斜带相分割。
5)  the east depression of North Yellow Sea
北黄海盆地东部坳陷
1.
The latest 2D seismic data indicate that the east depression of North Yellow Sea develops 4 significant unconformities: the unconformity between the Jurassic and Cretaceous, the one between the Mesozoic and Cenozoic, the one inside the Oligocene and the one between the Neogene and Paleogene.
在最新二维地震资料解释的基础上,对北黄海盆地东部坳陷的重要不整合面进行了研究,共识别出了4个重要不整合面;利用声波时差法和构造横剖面法,恢复了两期重要不整合面的剥蚀厚度;同时根据重磁资料及精细地震解释,对北黄海盆地东部坳陷的断裂特征作出了初步的研究,分析了主要断裂的形成期次及活动时间。
6)  Southwest Depression of Tarim Basin
塔里木盆地西南坳陷
1.
Along with Tajik Basin and the Southwest Southwest Depression of Tarim Basin, Alay Basin was one of the remnant basins on the north rim of the Tethys during the Late Triassic to Paleogene, it became a peripheral foreland basin in Miocene.
阿莱依盆地是特提斯北缘盆地群中的一个,晚三叠世—古近纪与相邻的塔吉克盆地、塔里木盆地西南坳陷基本连通,中新世以后才成为分隔的周缘前陆盆地。
补充资料:小北湖

小北湖位于济宁南郊六公里处,该湖原系我国北方最大的淡水湖,南四湖北端,为发展水产养殖业,于1973年筑堤围湖,并由此而得名,总面积1.8万亩,其中水面1.6万亩。东依古运河,西临京杭运河,成“双河抱湖”之势。小北湖是镶嵌在济宁大地上的一颗明珠,是独成一体的一块金三角。经过十几年的开发治理,集旅游、养殖于一体,已初具规模。小北湖水源充沛、日照充足、碧波荡漾,草丰鱼跃,荷花争艳,风景秀丽,气候宜人。湖内盛产驰名中外的武昌鱼、鲤鱼、鳜鱼、四鼻鲤鱼、甲鱼和虾、毛蟹等。湖区堤岸平直,一般水深1.5—2米,源底平坦,湖中有七个小岛。每年济宁市“荷花会”在此举行,吸引大批中外来客赏荷、垂钓、观光、旅游。

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