1) Longpan ramp valley
龙蟠谷地
1.
Then the formation mechanism of the old Longpan ramp valley was figured out.
通过河床钻孔并结合野外踏勘,确定了隐伏的龙蟠断裂在宽谷的切错位置,指出古龙蟠谷地是在上新世末早更新世初由龙蟠断裂发生逆断走滑和白汉场断裂的正断左旋并伴随断块的垂直升降活动而形成。
2) Longpan basin
龙蟠盆地
3) Panlong Oil Area
蟠龙探区
1.
Major factors controlling reservoir-quality of the Upper Triassic Chang 2 sandstones in the Panlong Oil Area;
蟠龙探区长2砂岩储层物性的控制因素
4) Longpan slope
龙蟠斜坡
5) Longpan right band
龙蟠右岸
1.
A seismic study of the deformable body on the Longpan right band of the Jinsha River;
金沙江龙蟠右岸变形体的地震学研究
6) Panlong Oilfield
蟠龙油田
1.
Diagenesis of Chang 2 Reservoir in Panlong Oilfield,Ordos Basin;
鄂尔多斯盆地蟠龙油田长2储层成岩作用研究
2.
Major factors controlling reservoir-quality of Chang 2 Reservoir in Panlong oilfield,Ordos Basin
鄂尔多斯盆地蟠龙油田长2储层物性主控因素分析
3.
Experiment Simulation of Micro-anisotropy of Yanchang Formation in F110-well Area in Panlong Oilfield
蟠龙油田F110井区延长组储层微观非均质性模拟
补充资料：因蟠国
因蟠国(いなば)(itaba)：属山阴道，俗称因州。石高约9万石(庆长时)。现在之鸟取县东部。古称稻叶，为古稻叶国，大化改新后改名因幡。废藩置县后本并入鸟取县。
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