1.
Geochemical Characteristics of Syenite and Its Genesis in the Luzong Basin
庐枞盆地正长岩类地球化学特征及成因探讨
2.
Geological and Geochemical Characteristics and Genesis of Longqiao Iron Deposit in Luzong Basin, Anhui, China
安徽庐枞盆地龙桥铁矿床地质地球化学特征和矿床成因研究
3.
Geological characteristics of siderites from Longqiao iron deposit in Luzong volcanic basin and their genetic significance
庐枞盆地龙桥铁矿床中菱铁矿的地质特征和成因意义
4.
SOME PETROCHEMICAL CHARACTERISTICS AND GENES IS OF SUBVOLCANIC ROCKS IN LUJIANG ZONGYANG BASIN, ANHUI PROVINCE
庐枞盆地次火山岩的若干岩石化学特征及其成因探讨
5.
The Deep Tectonics and Metallogenesis in Lu-Zong Volcanic Basin, Anhui, China
庐—枞火山岩盆地深部构造作用与成矿
6.
Study on CRS Stack of Complicated Surface and Application in Lu-Zong Basin
复杂地表共反射面叠加及在庐—枞盆地的应用
7.
Geology and Geochemical Characteristics and Mineralization Potential Estimation of Bajiatan Intrusion in Luzong Volcanic Basin, Anhui Province;
安徽庐枞火山岩盆地中巴家滩岩体的地质地球化学特征和成矿潜力评价
8.
A-TYPE GRANITES ALONG WITH SHOSHONITIC ROCKS IN THE LUZONG AREA
庐枞地区A型花岗岩类与橄榄安粗岩系研究
9.
THE RELATION BETWEEN THE DISTRIBUTION CHARACTERISTICS OF REGIONAL GEOPHYSICAL FIELD AND URANIUM MINERALIZATION IN LU-CONG REGION,ANHUI PROVINCE
安徽省庐枞地区地球物理场分布特征与铀矿化的关系
10.
Studies on Mesozoic A-type Granitoids and Their Rock Xenoliths in Lujiang-Zongyang Area, Anhui Province;
安徽庐枞地区中生代A型花岗岩类及其岩石包体研究
11.
AN EARLY CRETACEOUS PULL APART BASIN IN THE MIDDLE SECTION OF THE TAN LU
郯庐断裂中段的早白垩世拉分盆地(英文)
12.
The Depositional Response of Hefei Basin to the Activities of Tan-Lu Fault Zone;
合肥盆地对郯庐断裂带活动的沉积响应
13.
Research on deposition Response to Fault in the Su-Wan Segment of Tan-Lu Fault Zone and the Petroleum Geology Conditions of the Hefei Basin;
郯庐断裂带苏皖段断裂－沉积响应及合肥盆地油气地质条件研究
14.
Inversion mechanism of Meso-Cenozoic basins of southern Tan-Lu fault and its adjacent areas
郯庐断裂带南段及邻区中、新生代盆地的反转机制
15.
The Control on the Structure, the Sedimentary and Hydrocarbon Geological Condition of Hefei Basin in Tanlu Faulted Zone;
郯庐断裂带对合肥盆地构造、沉积及油气条件的控制
16.
Research on Relationship between Tectonic Evolution of the Tan-Lu Fault Zone and Adjacent Basins
郯庐断裂带构造演化特征及其与相邻盆地的关系
17.
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。
18.
The compressive activities from the earliest Neogene closed the above mentioned basins.
晚第三纪初期起动的挤压活动 ,使郯庐断裂带上的断陷盆地同步抬升和闭合 ;