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1)  East Sichuan
川东
1.
Reservoir features and controlling factors of J_1-J_2~2 Members of Fuxingchang in East Sichuan;
川东复兴场嘉一—嘉二~2储集特征及控制因素研究
2.
Imaging technique of seismic data from complicated steep structure area in east Sichuan.;
川东高陡复杂构造地震资料成像技术
3.
Discussion on Tan Handicrafts Co.,Ltd Entering into Natural Gas Market of East Sichuan;
从“谭木匠”入主下川东天然气市场谈起
2)  Eastern Sichuan Basin
川东
1.
In the Eastern Sichuan Basin the study of hydrocarbon-generating history of the Upper Permian source rocks has not well done up to now.
现今川东上二叠统烃源岩生烃史研究具有局限性。
2.
On this basis,the palaeokarst reservoirs development controlling factors in eastern Sichuan Basin are analysed and it is put forward that structure,climate,lithology,strata,ancient terrain,hydrogeologic conditions and different karst morphological forms influenced or even controlled the development and regional distribution of palaeokarst reservoirs.
作为川东地区最重要的天然气储集类型之一的石炭系黄龙组古岩溶型储层,业已引起众多油气地质工作者的重视。
3.
The initial application of the calibrated models in Wubaiti gas field in eastern Sichuan Basin suggests that Carboniferous paleo-reservoir cracked to gas mainly during 170~150 Ma.
为探讨川东五百梯气田石炭系黄龙组气藏的成藏史,利用金管实验装置,在高压、恒速升温的条件下对四川盆地源岩抽提物样品进行了热解成气实验,结合气相色谱和碳同位素分析,得到了甲烷生成率、甲烷碳同位素与实验温度和升温速率的关系。
3)  Eastern Sichuan
川东
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。
2.
In eastern Sichuan, Carboniferous strata are intensely folded and faulted, and complete anticlines are rare; so gas pools are generally non-anticlinal traps.
川东地区石炭纪的构造褶皱强烈,断裂发育,完整背斜很少,气藏一般赋存在背斜圈闭内。
4)  Dongchuan
东川
1.
Development of digital disaster reduction system for debris flow in urban district of Dongchuan;
东川城区泥石流数字减灾系统的开发
2.
Assessing Study of City Mud-Rock Flow Destruction——A Case of Dongchuan,Yunnan;
城市泥石流灾害易损性评价研究——以云南省东川区为例
3.
Construction of Ecological Environment and Debris Flow Control in Dongchuan;
东川生态环境建设与泥石流综合治理
5)  northeastern Sichuan
川东北
1.
Diagenesis and pore evolution of the oolitic shoal reservoir in the Feixianguan Formation in northeastern Sichuan;
川东北飞仙关组鲕滩储层成岩作用和孔隙演化
2.
Distribution and accumulation of materials in shoal-reef compound gas deposits and reservoir characteristics——A case study of the Changxing-Feixian Formation in the Puguang gas field, northeastern Sichuan;
礁滩复合型气藏物质聚集分布及储层特征研究——以川东北地区普光气田长兴组—飞仙关组为例
3.
Exploration achievements and prospects of the Permian Triassic natural gas in northeastern Sichuan basin;
四川盆地川东北区二叠系—三叠系天然气勘探成果与前景展望
6)  Northeastern Sichuan basin
川东北
1.
Sequence-based lithofacies and paleogeography of Lower Triassic Feixianguan Formation in northeastern Sichuan Basin;
川东北地区飞仙关组层序-岩相古地理特征
2.
Sequence styles and hydrocarbon accumulation effects of carbonate rock platform in the Changxing-Feixianguan formations in the northeastern Sichuan Basin
川东北地区长兴组-飞仙关组碳酸盐岩台地层序充填结构及成藏效应
补充资料:川东竹海

远处的老龙洞口被隐藏在翠竹之中,洞内各种岩溶景观独特,保存完好,堪称世外仙境。

● 川东竹海

华蓥山是一座宝山,也是一座绿色大宝库,八百里华蓥山区到处可见绿装素裹的景色,尤为壮观的是川东竹海,那是一片片绿色的竹子,山风吹拂,恰似那绿色的海洋,把本来就雄伟壮丽的华蓥山装扮得更加俏艳俊靓。

川东竹海在华蓥山上有两处,一处在天池山一带,一处在大竹山一带。华蓥山竹林面积有数百万亩,品种有白夹竹、楠竹、斑竹、慈竹、方竹、辞、刺竹、冷竹、黄竹、苦竹、芒竹、水竹、观音竹等数十种,以白夹竹为最多。川东竹海是当年华蓥山游击队的天然掩体,他们在竹海中与敌人周旋战斗,夺取了一个又一个胜利。

在竹海深处的仰天窝花竹山上,生长着一片国内罕见的花竹,有绿杆绿槽竹、绿杆黄槽竹、黄杆黄槽竹、黄杆绿槽竹,其科研价值和观赏价值极高。全国著名竹类专家易国培教授深入此山认真考察研究,未定出学名,推测可能是白夹竹的变种。川东竹海,绿波荡漾,景色别致,风光宜人。

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