Results 41 to 50 of about 69 (60)
Some of the next articles are maybe not open access.
Quarterly Journal of Engineering Geology and Hydrogeology, 1987
Abstract The present study introduces some of the relationships that exist between the geomechanical and geological characteristics of the materials within the paleogeographical ambit of the Purbeck-Weald Facies, and takes into account the geological history recorded in the composition and structure of the formations that contain them.
C. Tomillo, A. Foyo
exaly +2 more sources
Abstract The present study introduces some of the relationships that exist between the geomechanical and geological characteristics of the materials within the paleogeographical ambit of the Purbeck-Weald Facies, and takes into account the geological history recorded in the composition and structure of the formations that contain them.
C. Tomillo, A. Foyo
exaly +2 more sources
Cretaceous Research, 2014
Abstract A set of samples from the Camarillas Formation (Barremian, Weald facies) in the Galve Sub-basin (Central Iberian Chain, north-east Spain) was studied to determine the origin of the abundant kaolinitic clays and their relationship to the sedimentary environment, palaeoclimate and diagenetic processes.
Alfonso Yuste +2 more
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Abstract A set of samples from the Camarillas Formation (Barremian, Weald facies) in the Galve Sub-basin (Central Iberian Chain, north-east Spain) was studied to determine the origin of the abundant kaolinitic clays and their relationship to the sedimentary environment, palaeoclimate and diagenetic processes.
Alfonso Yuste +2 more
exaly +2 more sources
Proceedings of the Geologists Association, 1997
The Clockhouse Rock Store [TQ 174 384] has for the past twenty years been a major source of Wealden insect fossils, but the presence of vertebrate remains has only been briefly documented. Nine distinct vertebrate-bearing facies are described here. Sedimentary structures in the sandstones indicate fluvial deposition.
exaly +2 more sources
The Clockhouse Rock Store [TQ 174 384] has for the past twenty years been a major source of Wealden insect fossils, but the presence of vertebrate remains has only been briefly documented. Nine distinct vertebrate-bearing facies are described here. Sedimentary structures in the sandstones indicate fluvial deposition.
exaly +2 more sources
2016
Quantifying the geometries of evaporite deposits at a <1 km scale is critical in our understanding of similar ancient depositional systems, but is challenging given evaporite mineral dissolution at surface conditions. Two high-resolution stratigraphic studies in mines provide insight into the geometries, dimensions, and spatial distributions of ...
openaire +2 more sources
Quantifying the geometries of evaporite deposits at a <1 km scale is critical in our understanding of similar ancient depositional systems, but is challenging given evaporite mineral dissolution at surface conditions. Two high-resolution stratigraphic studies in mines provide insight into the geometries, dimensions, and spatial distributions of ...
openaire +2 more sources
Weald Clay (Lower Cretaceous) palaeoenvironments in south-east England: molluscan evidence
Cretaceous Research, 1999Jonathan D Radley
exaly
The Wealden (non-marine Lower Cretaceous) of the Weald Sub-basin, southern England
Proceedings of the Geologists Association, 2012Jonathan D Radley
exaly

