1) Fuxin uplift belt
扶新隆起带
1.
Xinmiaoxi area is situated in the north slope of Fuxin uplift belt,south Songliao basin,where the main reservoirs are characteristic of thin and interbedded sandstone/mudstone that belong to outer frontal sedimentary facies of delta.
新庙西地区位于松辽盆地南部扶新隆起带北坡,主要储层为砂泥岩薄互层,属三角洲外前缘沉积相带,储层横向变化快,砂泥岩薄互层中砂、泥岩速度差别小,波阻抗反演不能有效地识别砂岩,因此预测砂泥岩薄互层储层难度较大。
2) the north slope of Fuxin uplift zone
扶新隆起带北坡
3) Fuxin uplift
扶新隆起
1.
Inclusion analysis indicates that Fuxin uplift and Changling sag separate away after major reservoir-forming stage of Fuyu oil layer, i.
包裹体分析结果表明,吉林油田扶新隆起和长岭凹陷是在青一段生烃高峰后和扶余油层主成藏期后才发生明显的“隆—凹”分异,即油气充注和成藏发生于扶新隆起大规模隆升之前。
4) uplift belt
隆起带
1.
Control of the Early Faulted Depression of Superimposed Basins on Uplift Belts and Depression Belts——A new explanation for the origin of uplift belts and depression belts in the northern Qaidam Basin;
叠合盆地早期断陷对隆起带与凹陷带的控制——柴北缘隆起带与凹陷带的成因新认识
5) palaeohigh belt
古隆起带
1.
The Carboniferous natural gas in eastern Sichuan is of cracked gas which had been accumulated, originally as oil, in Liangping-Changshou palaeohigh belt that was formed by Indosinian movement.
川东石炭系中的天然气属于油型气,初为原油,曾经聚集于印支运动中形成的梁平—长寿古隆起带里,形成油藏。
6) mole track
隆起带
1.
The ore forming concentrated province of Au Ag Pb deposits in Huashan—Xiongershan massif has a close spatial relationship with Mesozoic mole track and fault basin as well as Yanshanian granite batholites and small granite porphyry bodies.
华熊地块区金、铅、银矿床矿集区与中生代隆起带、断陷盆地、燕山期花岗岩基及小花岗斑岩体空间关系密切。
补充资料：扶扶
1.幼小貌。汉扬雄《太玄．礥》:"赤子扶扶，元贞有终。测曰:赤子扶扶，父母詹也。"范望注:"扶扶幼小之貌也。"一说，依慕之意。司马光集注:"扶扶，扳援依慕之意。"
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条