1) Denglouku Formation
登娄库组
1.
Depositional System and Petroleum Prospect of the Third Section of Denglouku Formation in Western Fault Depression of North Songliao Basin;
松辽盆地北部西部断陷登娄库组三段沉积体系及油气远景
2.
Sedimentary facies analysis of the lower part of Denglouku Formation in northern Xujiaweizi area,Songliao Basin;
松辽盆地北部徐家围子地区登娄库组下部沉积相分析
3.
Study on Sedimentary Microfacies of Denglouku Formation in Changling Gasfield;
长岭气田登娄库组沉积微相研究
2) the upper of Denglouku Formation
登娄库组顶部
3) third member of the Denglouku Formation
登娄库组三段
1.
The third member of the Denglouku Formation is a prospect area for the oil and gas resources in the Xujiaweizi subsidence, Daqing, northeastern China.
本文从沉积相、岩性和测井相入手，分析了下白垩统登娄库组三段岩性发育及相类型，并划分了层序旋回，识别出各旋回体系域归属。
4) Denglouku anticline
登娄库背斜带
1.
Based on the analysis test data about petroleum geology,geochemistry,geophysics, sequence stratigraphy comprehensively and the method of combining the data with the method of geological research and analysis,the authors have studied the hydrocarbon accumulation in the Denglouku anticline.
本文综合运用石油地质学、地球化学、地球物理、层序地层学等分析测试资料,通过地质研究、分析相结合的方法,对登娄库背斜带油气成藏进行了研究。
5) Denglouku Formation
登楼库组
1.
Parahorologinella, as a new genus, is proposed for accepting a kind of palynomorphs found from the Denglouku Formation revealed by the boreholes Yu-302 and Yu-102 drilling in Yushu, southeastern Songliao Basin.
,产于松辽盆地东南部登楼库组第三段。
2.
The Denglouku Formation is a suite of sedimentary rocks composed of mudstone and conglomerate, with a thickness possibly attaining 1000- 1500m in this district.
本文系统研究了松辽盆地南部梨树断陷登楼库组孢子花粉化石，计３９属６０种，描述１０属１６种。
3.
Based on the stratigraphic distribution,biostratigraphy and isotopic ages,the authors correlate Fuxin formation in Western Liaoning with Yingcheng and Denglouku formations in the Songliao Basin.
在系统总结古生物资料的基础上,结合区域岩石地层分布情况及近年来同位素测年资料,得出如下结论:阜新组中下部(高德层-孙家湾层)可与营城组对比,时代为巴列姆期—阿普特期;阜新组上部(水泉层)可与登楼库组下部(一、二段)对比,时代为阿普特期;登楼库组上部(三、四段)与阜新组顶部火山岩(张老公屯组)层位相当,时代为阿普特期—阿尔布期。
6) Loushanguan Formation
娄山关组
1.
A Study of Sequence Stratigraphy of the Loushanguan Formation in the Boundary Area Between Hunan and Guizhou Provinces;
湘黔交界娄山关组层序地层学研究
2.
There exists paleokarst unconformity on top of the Loushanguan Formation,western Hubei.
鄂西娄山关组顶部存在古岩溶不整合面，有众多陆上暴露和溶蚀标志，表明其产生受寒武纪末海平面下降事件的控制。
补充资料：明登
明登
德国西北部城市。在威悉河和中部运河交汇点，汉诺威以西58公里。人口7.6万（1984）。公元798年首见记载。公路和铁路交通中心，河港。工业以化学、纺织和服装、玻璃、机械制造为主，还有造纸、酿酒、陶器等厂。
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