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1)  East Fukang Slope
阜东斜坡带
1.
Forming conditions and main controlling factors of the Middle-Upper Jurassic lithologic traps on East Fukang Slope,Jungar Basin;
准噶尔盆地阜东斜坡带中上侏罗统岩性圈闭形成条件及成藏主控因素分析
2.
Analysis of seismic facies and prediction of sedimentary system of Shishugou Group on the East Fukang Slope of Zhungeer Basin;
准噶尔盆地阜东斜坡带石树沟群地震相分析及沉积体系预测
2)  Fudong slope
阜东斜坡
1.
Analyses of the characteristics of the hydrocarbon passage system and the hydrocarbon migration and accumulation modes of middle-up Jurassic in Fudong slope;
阜东斜坡带中上侏罗统输导系统发育特征及油气运聚模式分析
2.
Application of inversion techniques to the exploration of the lithologic reservoirs in the regions with low prospecting degree —taking the middle-upper Jurassic in Fudong slope as an example;
反演技术在低勘探程度区域岩性油气藏勘探中的应用——以阜东斜坡带中上侏罗统为例
3)  East Fukang Slope
阜东斜坡
1.
Prediction method of the lithologic traps in the low exploration-degree area with sparse wells:taking Shishugou Group on East Fukang Slope of Zhungeer Basin as an example;
稀井低勘探程度区块岩性圈闭预测方法分析——以准噶尔盆地阜东斜坡带石树沟群为例
2.
On the basis of integrated studies of seismic data, cores, well logs and palaeontological stratigraphy of the East Fukang Slope, Junggar Basin, six stratigraphic sequences or two tectonic sequences are recognized from the Jurassic System of the study area.
通过地震、钻测井及生物地层资料的综合研究 ,认为准噶尔盆地阜东斜坡区侏罗系发育 6套层序、两个构造层序。
4)  The east of FuKang slop-north SanTai area
阜东斜坡-北三台
5)  eastern slope
东斜坡带
1.
Determining hydrocarbon accumulation period and age by fluid inclusions on the eastern slope of Chengdao oilfield;
应用流体包裹体研究埕岛油田东斜坡带油气藏成藏期次与时间
6)  Wudong Slope
乌东斜坡带
1.
For Wudong Slope of Hailaer Basin, the research on systematic characteristics is very poor.
基于海拉尔盆地乌东斜坡带缺乏系统特征研究的现状,依据坡折带的成因类型、坡折带的产状变化和组合样式,应用坡折带理论研究证实:乌东斜坡带存在构造坡折、沉积坡折、侵蚀坡折3种类型;运用储层预测技术,发现沿斜坡带发育多套横向连片纵向叠置的扇体。
补充资料:万阜

浙江青田县万阜乡 邮编323907

万阜地处青田高地,山水自然清秀,民风自然淳朴,有青田的西藏之称。因海拔落差大,山川秀美,又有小黄山之称。万阜与文成县南田交界,(南田是刘基故里所在,“七十二福地南田居其一”说的就是此地!)南田山的形势,乃是“万山之巅,独开平壤数十里,号南田福地”。《洞天福地记》中记载说“古称七十二福地,南田居其一”。俗语云:“九都九条岭,条条通天顶。”古时山里连接外面世界的,便是山民在大山上开辟的条条山道。南田古称九都,古地名在九都内按水系又分为源,如源头、一源、二源、三源…...。历史变迁现在大都数已不按此叫法!只有小数还是按古地名的叫,如:源头、二源、三源、十源。万阜乡处于南田整个台体的外围,古时称为九源,为“九都九源”!位万阜的石赤岭便是“九都九条岭”之一!

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