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1)  Junggar southern margin-Turpan
准噶尔南缘-吐鲁番盆地
2)  Southern margin of Junggar basin
准噶尔盆地南缘
1.
Characteristics of structure transform zones in the fold-thrust belts on the southern margin of Junggar basin,Northwest China;
准噶尔盆地南缘褶皱-冲断带的构造变换带特征
2.
Geochemical behaviors of crude oil in the southern margin of Junggar basin;
准噶尔盆地南缘原油地球化学特征
3.
Basic characteristics and distribution rule of oil - gas reservoir forming assemblage in the southern margin of Junggar Basin;
准噶尔盆地南缘油气成藏组合特征及分布规律
3)  southern Junggar Basin
准噶尔盆地南缘
1.
Application of varying velocity mapping technique for mountain front in southern Junggar basin.;
准噶尔盆地南缘山前带构造变速成图
2.
Discussion on shooting factors in the foothill in southern Junggar Basin.;
准噶尔盆地南缘山前带激发因素分析
3.
Geophysical Response Relationship Study on Characteristics and Mechanisms of Overpressure in Southern Junggar Basin;
准噶尔盆地南缘超压地球物理特征与成因响应关系研究
4)  the southern Junggar Basin
准噶尔盆地南缘
1.
The petroleum geological exploration and research in the southern Junggar Basin has been focused mainly on the Permian and Jurassic petroleum systems.
准噶尔盆地南缘地区的油气勘探与石油地质研究长期以来以二叠系和侏罗系含油气系统为主。
2.
In the east part of the Southern Junggar Basin,the deep structural wedges at the mountain fronts,which are composed of several Paleozoic-Mesozoic fault-bend folds,propagated northward along the coal layer of middle Jurassic;all slip transferred southward along back thrusts,above which the first row of anticlinal belt developed.
准噶尔盆地南缘3排背斜内带的构造楔形体模式非常典型,并表现为"混序"的特征。
5)  Southern margin of the Junggar Basin
准噶尔盆地南缘
1.
The microstructures of fault gouge and tectonite in the Huo erguosi-Manas-Tugulu reverse fault zones along the southern margin of the Junggar basin are studied and twelve samples of gypsum,fault gouge and quartz veins were collected and dated by using the electronic spin resonance(ESR)method.
对准噶尔盆地南缘霍尔果斯-玛纳斯-吐谷鲁逆断裂带中的断层泥和构造岩显微构造进行了研究,并对断裂带中的石膏、石英脉和断层泥进行了ESR测年。
6)  southern Junggar Basin near north tianshan
准噶尔盆地南缘山前带
补充资料:吐鲁番盆地
吐鲁番盆地

    位于中国新疆维吾尔自治区东部。是博格达山和觉罗塔格间的陷落盆地  。东西长200千米,南北宽80千米  。面积3470平方千米。地势北高南低,中部的艾丁湖(觉洛浣)水面低于海面154米。为中国陆上最低点。是中国夏季最炎热地区,气温最高曾达48.9℃,40℃以上日数30多天,地面温度82.3℃ ,是沙煮蛋、石烙饼的地方,古有火洲之称。1961~1970年年均降水量3.9毫米,蒸发量3000毫米以上。风力强劲,夏季热风,吹枯作物。戈壁滩、沙漠发育。属荒漠地形,呈环状结构。盆地四周是一圈戈壁砾石带,高山冰川雪水流向盆地低处,在山前形成地下水库;东部有小片沙漠称库姆塔格(即沙山),沙丘不移动;北部火焰山前缘为泥沙旱三角洲,赖坎儿井灌溉,发展农业。全区共有坎儿井1100多条,井长3~30千米,灌溉70%的田地。盛产棉花、葡萄、哈密瓜。
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