Results 81 to 90 of about 831 (199)

Tectono-sedimentary evolution of upper Assam “inter-orogenic” peripheral foreland basin, India

Discover Geoscience
The northern periphery of the Indian craton is the leading edge of the under-thrusting continent in the continent–continent collision set up between the Indian and Eurasian plates.
S. K. Biswas, Gaurav Chauhan
doaj   +1 more source

Heavy mineral analysis of the Upper Cretaceous to Lower Eocene synorogenic formations of the Pieniny Klippen Belt (Šariš Unit, eastern Slovakia): new data from the Jar-2 borehole (Jarmuta-Proč Fm.) and outcrops (Malinowa Fm.)

Mineralia Slovaca
The study presents new results of heavy mineral analyses including detrital garnet, tourmaline and Cr-rich spinel chemical compositions from the synorogenic Maastrichtian-Ypresian Jarmuta-Proč Fm. of the Šariš Unit of the Pieniny Klippen Belt, penetrated
Jozef Madzin, Dušan Plašienka
doaj   +1 more source

Geology of Tunceli-Bingöl Region of Eastern Turkey

Bulletin of the Mineral Research and Exploration, 1965
This region is located in the Taurus orogenic belt of the highland district of Eastern Turkey. Lower Permian metasediments and Upper Permian suberystalline limestone are the oldest exposed formations of this region.
F. A. AFSHAR
doaj  

Comparison of support vector machine and neutral network classification method in hyperspectral mapping of ophiolite mélanges–A case study of east of Iran

Egyptian Journal of Remote Sensing and Space Sciences, 2017
Ophiolitic regions are one of the most complex geology settings. Mapping in these parts need broad and precise studies and tools because of the mixture rocks and confusion units.
Bahram Bahrambeygi, Hesam Moeinzadeh
doaj   +1 more source

Assessing provenance of Upper Cretaceous siliciclastics using spectral γ-ray record

Geologica Carpathica, 2015
The relationship between contents of clay minerals/grain size and spectral γ-ray record (concentrations of K, U and Th) in sediments is used for interpretation of sedimentary facies in wire-line logs.
Šimíček Daniel, Bábek Ondřej
doaj   +1 more source

Coastal Dinaric Flysch Belt: Paleotransport model for the Pazin Basin and the role of a foreland uplift.

Natura Croatica, 1996
Sedimentary infill of the Pazin Basin, Istria, shows that the Eocene foreland basin in coastal Dinarides received the detritus from the outer (Adriatic) side, and not only from the SW indicates the existence of a carbonate area, which was partly exposed and partly covered by shallow sea characterized by carbonate deposition. This high area embraced the
Babić, Ljubomir, Zupanič, Jožica
openaire   +1 more source

Hydrogeological Relationships of the Golubinka Karst Spring in Ljubač Bay, Dalmatia, Croatia

Geologia Croatica, 2006
The Golubinka spring is a typical karst spring situated in northernDalmatia, Croatia. The catchment area is mostly composed of limestonesof the Cretaceous and Palaeogene, with some dolomitic parts.Hydrogeological barriers are composed of flysch or ...
Ante Pavičić, Josip Terzić, Nicoletta Berović   +2 more
doaj   +1 more source

Sedimentology of some Triassic-Middle Jurassic(?) Siliciclastic Flysch Deposits, Northwest Baja California Norte, Mexico

, 1985
Thesis, (M.S.) Geological Sciences.About 40 kilometers south of Tecate in northwestern Baja California Norte, in the Vallecitos-San Marcos area, lies an unknown thickness of poorly exposed, pre-middle Cretaceous, probable Triassic-Middle Jurassic ...
Reed, James Bradly
core  

The Early Miocene residual flysch basin at the front of the Central Western Carpathians and its palaeogeographic implications (Magura Nappe, Poland) [PDF]

, 2018
In the Polish sector of the Magura Nappe, along the front of the Pieniny Klippen Belt, strongly tectonized calcareous flysch up to 1000 m thick is exposed.
Oszczypko-Clowes, Marta, Oszczypko, Nestor, Oszczypko, N., Sotak, Jan, Boratyn, Józef, Piecuch, A., Soták, J., Oszczypko-Clowes, M., Boratyn, J., Piecuch, Anna   +9 more
core   +1 more source

Late Cretaceous age of magmatism at Vršatec in the Pieniny Klippen Belt, Western Carpathians, Slovakia

Mineralogia
Volcanic rocks in the Pieniny Klippen Belt (PKB) of the Western Carpathians have been the focus of geologists for over a century (e.g. Uhlig, 1890; Małkowski, 1921). Miocene volcanism is most common in the PKB.
Bazarnik Jakub, Matejová Marína Molčan, Lenik Piotr, Plašienka Dušan, Potočný Tomáš, Pańczyk Magdalena   +5 more
doaj   +1 more source