Heavy minerals from sandstones belonging mostly to the Boryslav Sandstone and Kliva Sandstone members of the lower part of the Menilite Formation (Oligocene) in the northern part of the Skole Nappe, Polish Carpathians are characterized. In the study area, the sediments were deposited in the Rzeszów and Łańcut channel zones running from the northern margin of the basin. The most frequent heavy minerals in the sandstones examined include zircon, tourmaline, rutile, staurolite, kyanite and garnet. Single grains of andalusite, sillimanite, apatite, epidote, brookite and chrome spinel occur in some samples. The very small content of apatite is related to long, continental weathering in the source area, which is referred to the Paleozoic sediment...
The types, abundance and origin of non-opaque heavy minerals from 17 samples of sandstones and granu...
Throughout the Cretaceous, Tethyan oceanic branches gradually closed, and various ophiolites became ...
Detrital heavy minerals separated from the Malcov Fm. deposits (Magura Nappe) indicate their source ...
Heavy minerals from sandstones belonging mostly to the Boryslav Sandstone and Kliva Sandstone member...
Conventional and high-resolution analyses of heavy minerals from the gravity flow-deposited sandston...
The Futoma Member (Oligocene, Rupelian) of the Menilite Formation is present only in the northern pa...
The study focused on the chemistry of detrital garnet and tourmaline from sediments of the Boryslav ...
Heavy mineral assemblages from the infill of Jurassic pre-Callovian palaeokarst in the Czatkowice Qu...
The types, abundance and origin of non-opaque heavy minerals from 17 samples of sandstones and granu...
Heavy mineral assemblages of the Upper Cretaceous-Palaeocene sandstones of the Polish part of the Ma...
The Futoma Member (Oligocene, Rupelian) of the Menilite Formation is present only in the northern pa...
Heavy min er als from sand stones be long ing mostly to the Boryslav Sand stone and Kliva Sand stone...
The composition of heavy-mineral assemblages is one of the main textural features of sediments becau...
Przedstawione opracowanie jest kolejną próbą porównania, a także ustalenia genezy piaskowców z Filip...
Garnet in heavy-mineral assemblages, occurring in sandstones of the Campanian–Maastrichtian part of ...
The types, abundance and origin of non-opaque heavy minerals from 17 samples of sandstones and granu...
Throughout the Cretaceous, Tethyan oceanic branches gradually closed, and various ophiolites became ...
Detrital heavy minerals separated from the Malcov Fm. deposits (Magura Nappe) indicate their source ...
Heavy minerals from sandstones belonging mostly to the Boryslav Sandstone and Kliva Sandstone member...
Conventional and high-resolution analyses of heavy minerals from the gravity flow-deposited sandston...
The Futoma Member (Oligocene, Rupelian) of the Menilite Formation is present only in the northern pa...
The study focused on the chemistry of detrital garnet and tourmaline from sediments of the Boryslav ...
Heavy mineral assemblages from the infill of Jurassic pre-Callovian palaeokarst in the Czatkowice Qu...
The types, abundance and origin of non-opaque heavy minerals from 17 samples of sandstones and granu...
Heavy mineral assemblages of the Upper Cretaceous-Palaeocene sandstones of the Polish part of the Ma...
The Futoma Member (Oligocene, Rupelian) of the Menilite Formation is present only in the northern pa...
Heavy min er als from sand stones be long ing mostly to the Boryslav Sand stone and Kliva Sand stone...
The composition of heavy-mineral assemblages is one of the main textural features of sediments becau...
Przedstawione opracowanie jest kolejną próbą porównania, a także ustalenia genezy piaskowców z Filip...
Garnet in heavy-mineral assemblages, occurring in sandstones of the Campanian–Maastrichtian part of ...
The types, abundance and origin of non-opaque heavy minerals from 17 samples of sandstones and granu...
Throughout the Cretaceous, Tethyan oceanic branches gradually closed, and various ophiolites became ...
Detrital heavy minerals separated from the Malcov Fm. deposits (Magura Nappe) indicate their source ...