1) The west slop of Qianliyuan Depression
前梨园凹陷西坡
2) QLY area of Dongpu depression
东濮凹陷前梨园
3) Qianliyuan depression
前梨园洼陷
1.
The natural gases in Baimiao area mainly stemmed from the Tertiary Hydrocarbon source rock and Permo-Carboniferous coal-bearing strata in Qianliyuan depression.
应用多种方法确定了杜桥白地区深层天然气的来源 ,研究表明白庙地区天然气主要来源于前梨园洼陷第三系烃源岩和石炭—二叠系煤系地层 ,靠近兰聊断裂带构造高点 ,浅层 Es下2 — Es23气层具有较高的4 0 Ar/ 36 Ar比值 ,为煤型气及混合气 ,而远离兰聊断裂带 ,且处于构造低部位的 Es1 3— Es4 3气层具有较低的 4 0 Ar/ 36 Ar比值 ,为油型气 ;桥口构造 Es33、Es4 3段气层主要为油型气 ;杜寨地区 Es33段气层为油型气 ,来自于 Es33段气源岩。
2.
Being controlled by Lanliao fault on the margin, Qianliyuan depression continues developing to provide the necessary foundation of the formation of deep basin gas accumulations.
前梨园洼陷受凹陷边界兰聊断裂控制 ,持续发育 ,为深盆气形成提供了必要的基础。
4) Lishu depression
梨树凹陷
1.
Five kinds of fault activity model are summedup by recovering the tectonic developing history of Lishu depression and by studying the main controling fault s nature,formation causes,present property as well as evolutive history, through analysing oil and gas accumulation and non-oil and gas accumulation,as well as the relation of fault and petroleum generating, migrating,accumulating.
通过恢复梨树凹陷构造演化历史，对本区控制断陷演化的主要断裂的性质、成因、现今特征、发育历史进行分析，总结出断裂活动的５种模式。
2.
By using the data of seism data, log data, core information, the framework of sequence strata and sedimentary facies in LiShu depression are analyzed and studied deeply, also the advantageous targets are researched and forecasted primarily.
本文综合采用层序地层学、沉积学、地震地层学等最新理论和方法,运用地震、测井、录井、岩心等分析资料,对梨树凹陷地区的层序地层格架、沉积相进行了细致的分析和研究,并对有利区带进行了初步分析和预测。
5) clival pit
斜坡陷凹
6) Pear Garden(theatre) in the west
西方梨园
补充资料：幸梨园亭观打球应制（一作梨园亭子侍宴应制
【诗文】：
年光陌上发，香辇禁中游。草绿鸳鸯殿，花明翡翠楼。
宝杯承露酌，仙管杂风流。今日陪欢豫，皇恩不可酬。
【注释】：
【出处】：
全唐诗：卷54_11全唐诗：卷81_35
年光陌上发，香辇禁中游。草绿鸳鸯殿，花明翡翠楼。
宝杯承露酌，仙管杂风流。今日陪欢豫，皇恩不可酬。
【注释】：
【出处】：
全唐诗：卷54_11全唐诗：卷81_35
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