289 - 298 |
MICROBIAL DOLOMITES FROM CARBONATE-EVAPORITE SEDIMENTS OF THE COASTAL SABKHA OF ABU DHABI AND THEIR EXPLORATION IMPLICATIONS Sadooni FN, Howari F, El-Saiy A |
299 - 318 |
ORGANIC GEOCHEMISTRY, BURIAL HISTORY AND HYDROCARBON GENERATION MODELLING OF THE UPPER JURASSIC MADBI FORMATION, MASILA BASIN, YEMEN Hakimi MH, Abdulah WH, Shalaby MR |
319 - 337 |
RELATIONSHIP BETWEEN ORGANIC MATTER, SULPHUR AND PHOSPHATE CONTENTS IN UPPER CRETACEOUS MARINE CARBONATES (KARABOGAZ FORMATION, SE TURKEY): IMPLICATIONS FOR EARLY OIL GENERATION Inan S, Ugur FA, Inan T, Yalcin MN, Mann U |
339 - 353 |
HYDROCARBON POTENTIAL OF THE LATE CRETACEOUS GONGILA AND FIKA FORMATIONS, BORNU (CHAD) BASIN, NE NIGERIA Alalade B, Tyson RV |
345 - 363 |
EARLY TOARCIAN SOURCE-ROCK POTENTIAL IN THE CENTRAL HIGH ATLAS BASIN (CENTRAL MOROCCO): REGIONAL DISTRIBUTION AND DEPOSITIONAL MODEL Bodin S, Frohlich S, Boutib L, Lahsini S, Redfern J |
355 - 369 |
SOURCE ROCK POTENTIAL AND ORGANIC GEOCHEMISTRY OF CENOMANIAN-TURONIAN BLACK SHALES, WESTERN TAURUS, SW TURKEY Kara-Gulbay R, Yurtsever TS, Korkmaz S, Demirel IH |
365 - 385 |
LIGHT HYDROCARBONS IN SOIL GAS ABOVE PROSPECTIVE OIL- AND GAS-BEARING STRUCTURES: POMERANIAN SYNCLINORIUM, NW POLAND Sechman H, Dzieniewicz M, Nowicka A |
371 - 386 |
DEPOSITIONAL ENVIRONMENTS AND SEQUENCE STRATIGRAPHY OF THE EARLY TRIASSIC KANGAN FORMATION IN THE NORTHERN PART OF THE PERSIAN GULF: IMPLICATIONS FOR RESERVOIR CHARACTERISTICS Peyravi M, Kamali MR, Kalani M |
387 - 403 |
SEQUENCE STRATIGRAPHY AND RESERVOIR CHARACTERISTICS OF THE TURONIAN-CONIACIAN KHASIB FORMATION IN CENTRAL IRAQ Al-Qayim B |
387 - 409 |
HYDROCARBON HABITAT OF THE SEDANO TROUGH, BASQUE-CANTABRIAN BASIN, SPAIN Beroiz C, Permanyer A |
411 - 428 |
SYNDEPOSITIONAL TECTONIC CONTROLS AND PALAEO-TOPOGRAPHY OF A PERMIAN TIGHT GAS RESERVOIR IN NW GERMANY Vackiner AA, Antrett P, Stollhofen H, Back S, Kukla PA, Barle C |
429 - 440 |
PETROLEUM ACCUMULATIONS AND INVERSION STRUCTURES IN THE XIHU DEPRESSION, EAST CHINA SEA BASIN Yang FL, Xu X, Zhao WF, Sun Z |