Titlebook: Basin Analysis in Petroleum Exploration; A case study from th Paul G. Teleki,Robert E. Mattick,János Kókai Book 1994 Springer Science+Busin

Interferons

,Politics and Policies, 1980–2000,ltaic progradation in a deep lacustrine basin. Cores, well logs and seismic profiles were used to investigate the sedimentologic processes, the paleoenvironments of deposition, and the history of basin filling. A gradual termination of middle Miocene (Badenian-Sarmatian) shallow-marine bioclastic de

絆住

Schooling and Literacy before World War II,ression of the Paratethys Sea is marked by conglomerate and/or breccia that is present almost everywhere where Miocene deposits occur. The Miocene sequence is 0-275 m thick, where penetrated by wells in the Békés basin; however, in the deepest parts of the basin the sequence is inferred to be more t

cumulative

Michael Dobbins,Christoph Knillomprise the Pannonian sequence or group. Interpretation of well data and seismic reflection data indicates that these rocks were deposited in a wide range of depositional environments ranging from deep-basinal brackish/lacustrine to basin slope to shallow lake and delta plain to alluvial plain. Seis

Dorsal

Michael Dobbins,Christoph Knilleen correlated and placed in relative stratigraphie positions by means of seismic profiles. Polarity zonations for two 2-km-thick cored sections were correlated with the polarity time scale for much of late Miocene time, and two cored sections, 1.2 km thick, were correlated with the polarity time sc

glacial

有特色

Higher Education Governance in East Asiaich the oils were generated, establish crude oil-source rock correlations and infer secondary migration routes in the basin. The aim of the study was to provide a geochemical underpinning which could be used to predict the occurrence of undiscovered oil accumulations..Organic geochemical characteriz

jumble

Jung Cheol Shin,Soo Jeung Lee,Yangson Kimposition and stable carbon isotope data indicate that most of the flammable gases were derived from humic kerogen contained in source rocks located in deep parts of the basin. Depths of gas generation and vertical migration distances were estimated by comparing rock maturity and carbon isotopic comp

混合

可以任性

Jung Cheol Shin,Soo Jeung Lee,Yangson Kimd smaller continental fragments following southward subduction of Tethyan ocean floor. A set of discrete basins, whose development was dominated by extensional listric and wrench faults, formed inside the Carpathian loop in middle Miocene time. The basin-forming tectonic activity culminated in middl

reptile