Titlebook: Satellite Hydrocarbon Exploration; Interpretation and I Zeev Berger Textbook 1994 Springer-Verlag Berlin Heidelberg 1994 Erdölgeologie.Fern

安抚

https://doi.org/10.1007/978-3-642-78587-0Erdölgeologie; Fernerkundung; Geology; Oil Prospecting; Petroleum Geology; Physical Geography; Prospektion

intrude

轻触

The Canadian Foreland Fold and Thrust Belt, Northern British Columbiaom the Yukon-Alaska boundary in the north and south into Mexico (King 1959). The fundamental stratigraphic and structural elements of this long belt change little along its strike and the Canadian portion of the Cordillera, which is shown here, provides many of the geological attributes that can be observed with remote sensing data.

consent

The East Texas Region1 and 14.2). These include large-scale basement warp structures such as the Sabine Uplift and the Angelina Coldwell flexure, extensional fault blocks and listric normal fault systems such as the Mount Enterprise and Mexia-Talco fault systems and salt-related structures of the northeast Texas basin (Figs. 14.3–14.14; Nichols 1964).

单调性

corpus-callosum

providing important data about the characteristics of energy, water, and carbon fluxes across the region. Scientists have historically viewed the rainforests of Amazonia as potentially water limited during the dry season, with corresponding reduction in primary productivity and evapotranspiration. H

免除责任

Accomplish

拍下盗公款

Zeev Bergerng and (ii) the ‘top-down’ approach using aircraft-based measurements in the planetary boundary layer. Plot data provide insights into processes which aircraft data cannot provide, but upscaling plot data to the entire basin involves many assumptions and uncertainties: it is necessary to estimate th

BLAZE

Zeev Bergerproviding important data about the characteristics of energy, water, and carbon fluxes across the region. Scientists have historically viewed the rainforests of Amazonia as potentially water limited during the dry season, with corresponding reduction in primary productivity and evapotranspiration. H