1) Yuanjiang sag
沅江凹陷
1.
Using the data obtained from seismic, well log, and assaying, the research is conducted on sequence stratification and sedimentary facies of Taoyuan Formation, Yuanjiang Formation, Hanshou Formation, and Xinhekou Formation of Paleogene inYuanjiang sag in the Dongtinghu Basin.
通过地震、测井和分析化验等资料,对洞庭湖盆地沅江凹陷古近系古新统桃源组及始新统沅江组、汉寿组及新河口组进行层序地层和沉积相研究,首先可将古近纪划分为2个Ⅲ级层序、5个体系域,桃源组和沅江组构成层序I,汉寿组和新河口组构成层序Ⅱ。
2.
The Paleogene in Yuanjiang sag of the Dongting basin occurs as a NE-trending quasi-dustpan-shaped sag being faulted in the southeast and onlapping in the northwest.
洞庭盆地沅江凹陷古近系总体表现为一个北东向展布的东南断裂、西北超覆的断陷—断坳型准箕状凹陷。
3) Jiangling depression
江陵凹陷
1.
Thermal Evolutional History of Hydrocarbon Source Rocks in Jiangling Depression;
江陵凹陷烃源岩热演化史探讨
2.
Diagenesis and pore evolvement of the lower member of Xingouzui formation sandstone in Jiangling depression;
江陵凹陷新沟嘴组下段砂岩成岩作用及孔隙演化
3.
Genesis of heterogeneity of secondary pores in deep reservoir of Jiangling Depression;
江陵凹陷深层储层次生孔隙非均质性成因
4) Qianjiang depression
潜江凹陷
1.
Main controlling factors and exploration direction of subtle oil reservoirs in Qianjiang depression;
潜江凹陷隐蔽油藏成藏主控因素及勘探方向
2.
On understanding of the oolitic limestone oil-bearing characteristics in Qianjiang Formation of Qianjiang Depression;
对潜江凹陷潜江组鲕状灰岩含油特征的认识
3.
Relationships between Formation Water Chemical Characteristics and Hydrocarbon Generation in the South of Qianjiang Depression;
潜江凹陷南部地层水化学特征与油气成藏的关系
5) Qianjiang sag
潜江凹陷
1.
Exploration technology for subtle reservoirs in Qianjiang sag.;
潜江凹陷隐蔽油藏勘探技术
2.
Sedimentary microfacies and evolution of the Qianjiang Formation of Paleogene at Wangchang area in Qianjiang Sag,Jianghan Basin;
江汉盆地潜江凹陷王场地区古近系潜江组沉积微相及其演变
3.
Palaeogeomorphology and origin of sandbodies of the Member 3 of Qianjiang Formation in Qianjiang Sag,Jianghan Basin
江汉盆地潜江凹陷潜三段古地貌与砂体成因分析
6) Jiangling Sag
江陵凹陷
1.
Prolific Hydrocarbon Generating Depression and Near-Source Type Accumulation in the Southwest Area of Meihuaiqiao Depression of Jiangling Sag
江陵凹陷西南部梅槐桥富生烃洼陷及近源油气成藏
2.
Salt structure is very development in Jiangling sag.
含盐盆地具有丰富的油气资源 ,盐构造与油气藏存在密切关系 ,江陵凹陷盐构造非常发育 ,对油气聚集具有重要的影响 :①盐构造及其伴生构造是油气聚集的有利空间场所 ;②盐构造形成可改变流体动力系统并为油气运移、聚集提供网络通
补充资料:沅江
沅江 位于中国湖南省西部 。源出贵州省东南部 。分南北两源:南源龙头江,源出都匀市云雾山鸡冠岭;北源重安江,源出麻江县北之大山。两水汇合后称清水江。东流至黔城会沅水后,水量大增,始称沅江。东北流经辰溪县、沅陵县、常德市,在德山入洞庭湖。长1033千米,流域面积8.92万平方千米。河网发育,呈羽状水系。主要支流有沅水、辰水、武水、酉水、渠水、巫水、溆水等。黔城以上为上游,属贵州高原(云贵高原),峰回水转,河道弯曲,水势湍急;黔城至沅陵为中游,滩陡礁多浪险;沅陵以下属下游,山势低落,至桃源河流入平原,江阔波平,舟行通畅。多年平均径流量677亿立方米。水力资源丰富 ,已在酉水中游建成的凤滩电站装机40万千瓦。贵州省天柱县远口镇以下可通航。 |
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