1) Hanjiang Sag
韩江凹陷
2) 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
3) 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
4) 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
5) 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
6) the shelf basin of the East China Sea
长江凹陷
补充资料:韩江
韩江 位于中国广东省东部。上游有两源:北源汀江 ,又名鄞江,发源于福建省长汀县东北上坪山,自北向南流。南源梅江发源于广东省紫金县白山东,自南向北偏东流。两江在大埔县三河坝汇合后始称韩江,南流到澄海市分成东、西、北3支,由5个口门流入南海,全长428千米,流域面积3万平方千米。梅江和汀江从各自源头到三河坝分别长为300千米和260千米,由于梅江河长大于汀江,故多将梅江作为韩江的正源。汀江属山溪性河流,多峡谷、险滩,径流丰富,多年平均径流深965毫米(溪口站)。梅江蜿蜒于广谷和盆地中,多年平均径流深760毫米(横山站)。韩江流域水力资源理论蕴藏量为201.44万千瓦,实际可开发量为142万千瓦,以汀江流域水力资源最为丰富。汀江自上杭可上溯通航汽轮50千米;梅江从梅州可以上溯汽轮至五华。梅州以下和韩江可以通2.5~30吨级轮船。 |
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参考词条