1.
THE EVOLUTION OF THE RIFTED OCEANIC BASIN DUE TO LITHOSPERIC STRETCHING IN YUNNAN, GUIZHOU AND GUANGXI PROVINCES DURING THE LATE HERCYNIAN TO MIDDLE INDOSINIAN STAGE
滇黔桂晚海西—中印支伸展裂谷海盆地的演化
2.
GENETIC ANALYSES OF EOGENE RIFT STRATA IN THE SHELF BASIN,EAST CHINA SEA
东海陆架早第三纪裂谷盆地地层成因浅析
3.
intracratonic rift-style basin
克拉通内裂谷型盆地
4.
Discussion of Basin-fill Mechanism during Eogene Rifting Phase in Oujiang Trough, the East China Sea
东海瓯江凹陷早第三纪裂谷期盆地充填机制探讨
5.
Numerical models of the tectono-thermal evolution of rift basins and their applications to the Northern South China Sea
裂谷盆地构造热演化的数值模型及在南海北部的应用
6.
Lithosphere Stretching Model of Deep Water in Qiongdongnan Basin,Northern Continental Margin of South China Sea,and Controlling of the Post-Rift Subsidence
琼东南盆地深水区岩石圈伸展模式及其对裂后期沉降的控制
7.
Subsidence process of extensional basin in post-rift period and its dynamic setting
伸展型盆地裂后期沉降过程及其动力学背景研究
8.
Liaohe basin is a rift basin developed in the Mesozoic and Cenozoic.
辽河盆地是中、新生代发育起来的裂谷盆地。
9.
Study on Reservoir formation in Lower Cretaceous, Erlian Basin, Northeast Rift
东北裂谷二连盆地下白垩统成藏研究
10.
The Bohai bay Basin is a Cenozoic rifting one.
渤海宵盆地是一个新生代裂陷盆地。
11.
The characteristics of the Mesozoic volcanic rock in the Songliao Basin reflect that this basin is a backarc rift basin.
松辽盆地中生代火山岩特征反映了该盆地为弧后裂谷盆地的性质。
12.
Transporting condition of faults required in formation of large and medium gas fields with high efficiency in rift basin
裂谷盆地高效大中型气田形成的断裂输导条件
13.
Study of Seismic Prediction to Fractured Reservoir in Songliao Basin and Hailaer Basin;
松辽盆地和海拉尔盆地裂缝储层地震预测研究
14.
The distribution of Xar Moron River Fault under Songliao Basin
西拉木伦河断裂在松辽盆地下部的延伸
15.
Hydrocarbon prospective evaluation of Albert rift basin-An example of evaluation about least explored basins.
艾伯特裂谷盆地含油气远景评价──极低勘探程度盆地评价实例
16.
Preliminery Studies on the Late Quaternary Activity of the Western Margin Fault of Gulu Basin,Tibet
谷露盆地西缘断裂晚第四纪活动初步研究
17.
Study on the New Active Characters of Western Margin Fault of Gulu Basin,Tibet
西藏谷露盆地西缘断裂新活动特征研究
18.
The Tan Lu fault zone turned into a huge extensional structure during Late Cretaceous to Eogene, leading to a series of development of fault bounded basins.
晚白垩世 早第三纪郯庐断裂带转变成巨型的伸展构造 ,普遍控制发育了断陷盆地。