...Fig. 6 ( a ) Garnet-staurolite paragneiss of the Texel Complex with a mylonitic fabric. Shear zone close to the Texel-Schneeberg boundary, SW of the Hohe Wilde; ( b ) Mylonitic marbles. The thin black layers are mainly formed by white mica and quartz. NW of the Stettiner Hütte, along the path...

...Fig. 1. Left: Geological sketch of the area west of the Tauern Window, including the sample location (arrow) in the Texel Complex. SC – Silvretta Complex; ÖSC – Ötztal-Stubai Complex; CC – Campo Complex; Northern Calcareous Alps in gray. Right: Topographic map including the sample location (black...

... in (A)] showing the Texel Complex as part of the KWNS ( cf . Pomella et al . 2016 ) and the adjacent tectonic units; stippled white area within the Texel Complex represents location of the pegmatite field as delimited by Sassi (1969) ; black star gives approximate location of the pegmatites investigated...

... characterized based on a planar texel (textural element) using a gray level co-occurrence matrix. I extend the concepts to a 3D seismic domain, where reflection amplitudes are visualized by voxels (volume picture elements). By evaluating a voxel co-occurrence matrix (VCM) based on a cubic texel at each...

... location in the image space. At each sample location, texture is characterized by using a small analysis window, which is usually called a texture element or texel by workers in this area to imply its functionality (e.g., Haralick et al., 1973 ; Reed and Hussong, 1989 ; Gao et al., 1998 ; Gao, 1999a...

...Satinder Chopra; Vladimir Alexeev Abstract In this study, texture attribute analysis application to 3D surface seismic data is presented. This is done by choosing a cubic texel (texture element) from the seismic data to generate a gray-level occurrence matrix, which in turn is used to compute...

... uses a pan-and-tilt scanner head that is somewhat slower than the USGS system Figure 3 . Scan times for Figure 3. The USU LIDAR unit scanning a landslide headscarp near Yamakoshi. Note the color Texel camera mounted on the top of the unit. TERRESTRIAL-LIDAR VISUALIZATION OF SURFACE AND STRUCTURAL...

... in crystalline basement rocks of the Eastern Alps in northern Italy. These crystalline rocks belong to the Austroalpine Texel Complex, which represents the westernmost portion of the Koralpe-Wölz high-pressure nappe system (KWNS) ( Schmid et al . 2004 ). The pegmatites form decimeter- to meter-wide concordant...

... and Blaser nappes; Figure 2 ). The Schneeberg and Texel units represent parts of the Apulian plate that experienced high-P/low-T metamorphic conditions during the Cretaceous orogeny ( Figure 2 ) [ 57 , 58 ]. Based on a structural analysis, it was recently suggested that the Ötztal-Stubai Complex...

.... ; and Sölva , H. 2006 . Tracing the high pressure stage in the polymetamorphic Texel Complex (Austroalpine basement unit, Eastern Alps): P–T–t–d constraints . Mineral. Petrol. 88 : 269 – 296 . Hacker , B. R. ; McClelland , W. C. ; and Lihou , J. C. 2006 . Ultrahigh-pressure...

... rocks, is highly structured, both by regional tectonic movements and by local salt mobility. Regional positive features, such as the Mid-North Sea high, the Ringkobing-Fyn-Falster high, and the Texel high divide the North Sea into several subbasins and have influenced regional sedimentation. Three major...

...Fig. 1. Geological map of the Schneeberg Complex. The location of the study area within the Seewertal is indicated. Geological overview at the upper left corner: SC (Schneeberg Complex); TG (Texel Group). Age data and mineral zones are taken from Thöni (1981) . ...

... to a broadly east–west-oriented belt of carbonate platforms that fringed the Old Red continent ( Korn 2008 ). The northwestern part of the Northwest European Carboniferous Basin was characterized by a major delta complex (Yoredale facies), which might have prevented the development of carbonate platforms...