"Core description and depositional analysis of the terrigenous Triassic section in the Norsk Hydro 7124 / 3-1 well; Barents Sea, Norway . " Geological Science Group Rept ., TSR 88-0039, April, 1988.
22.
Non-karstic landforms includes three types : The middle and low dome-block mountains developed in intrusive magmatic massifs; The middle denudation-structural mountain belts developed in terrigenous rocks of Cretaceous age; and The low block-denudational mountain belts developed in other terrigenous rocks.
23.
Non-karstic landforms includes three types : The middle and low dome-block mountains developed in intrusive magmatic massifs; The middle denudation-structural mountain belts developed in terrigenous rocks of Cretaceous age; and The low block-denudational mountain belts developed in other terrigenous rocks.
24.
When bioclasts are in its rock formation, meaning that they have gone through all the stages that sediments go through to reach its final phase, a whole rock unit, it is accompanied and mixed with variable amount of terrigenous material, glauconite particles and also phosphate grains.
25.
Its fossilized remains were retrieved in the late sixties and subsequent years from reworked reddish, massive or crudely stratified silty-sandy clays ( terrae rossae ), which partially fill the paleo-karstic fissures in the Mesozoic limestone substrate and that are on their turn overlain by Late-Pliocene-Early Pleistocene sediments of a subsequently marine, shallow water and terrigenous origin.
26.
"' Diamictite "'(; from Ancient Greek " ??? " ( dia-) : " through " and " ��????? " ( meikt�s ) : " mixed " ) is a type of lithified sedimentary rock that consists of nonsorted to poorly sorted terrigenous sediment containing particles that range in size from clay to boulders, suspended in a terrigenous gravel suspended in either a mud or sand matrix.
27.
"' Diamictite "'(; from Ancient Greek " ??? " ( dia-) : " through " and " ��????? " ( meikt�s ) : " mixed " ) is a type of lithified sedimentary rock that consists of nonsorted to poorly sorted terrigenous sediment containing particles that range in size from clay to boulders, suspended in a terrigenous gravel suspended in either a mud or sand matrix.
28.
From 1947 to 1950, he headed the Laboratory of Lithology and Geochemistry at UfNII . In 1949 Timergazin defended his thesis, " The terrigenous rocks of the Devonian-Bavlinsky Tuimazinsky oil region . " In 1950-1951, he was head of the Geological Department of UfNII before directing the Mining and Geology Institute of the BASSR until 1953 and heading the Laboratory of Petroleum Geology, Mining and Geological Institute ( now the Institute of Geology, Ufa Scientific Center of the Russian Academy of Sciences ).
