(paper pages 133-156) zagros active fold-thrust belt lies on the northern margin of the arabian continental crust it is a young fold-thrust mountain belt currently shortening, thickening and uplifting as a result of the collision of the arabian and iranian plates. rethickening of crust during collisional orogenies could have been carried out by reversal of fault motion along the mesozoic normal...

Identification of the geological facies and their distribution from seismic and other available geological information is important during the early stage of reservoir development (e.g. decision on initial well locations). Traditionally, this is done by manually inspecting the signatures of the seismic attribute maps, which is very time-consuming. This paper proposes an application of the Expec...

Erratum to “A novel tensor distribution model for the diffusion-weighted MR signal” [NeuroImage 37 (2007) 164–176] Bing Jian, Baba C. Vemuri,⁎ Evren Özarslan, Paul R. Carney, and Thomas H. Mareci Department of Computer and Information Science and Engineering, University of Florida, P.O. Box 116120, Gainesville, FL 32611, USA Section on Tissue Biophysics and Biomimetics, LIMB, NICHD, National In...

The process of risk assessment and investigation potentially contaminated soil groundwater is highly dependent on a proper understanding the geological hydrogeological conditions investigated site. current paper aims at identifying general landfill areas around Bucharest city based interpretations data available in research articles, books, public reports, maps. Several samples were collected, ...

Mapping of geological variables in the Croatian part Pannonian Basin System (CPBS) is mostly based on small input datasets. In case analyzed hydrocarbon field "B", reservoir "K", due to complex structure and pronounced tectonics, interpretations are restricted several blocks, where each has very limited dataset. The porosity (19 data) permeability (18 were analyzed. applied interpolation method...

introduction the aqkand cu occurrence, 48 km north of zanjan, is located in the tarom subzone of the western alborz-azerbaijan structural zone. apart from small scale geological maps of the area, i.e., 1:250,000 geological maps of bandar-e-anzali (davies, 1977) and 1:100,000 geological maps of hashtjin (faridi and anvari, 2000) and a number of unpublished perlite exploration reports, prior to t...

this work aims to extract the mineralogical constituents of the lahroud hyperion scene situated in the nw of iran. like the other push-broom sensors, hyperion images suffer from spectral distortions, namely the smile effect. the corresponding spectral curvature is defined as an across-track wavelength shift from the nominal central wavelength, and alters the pixel spectra. the common “column me...