Posebna izdanja (Srpdka kraljevska akademija), Том 296 |
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Страница 75
... also the colour index is not as high as in the basalts . These rocks have also a positive qz , which is also a feature by which they differ from the basalts . Although it is difficult to place them under one heading into a classi ...
... also the colour index is not as high as in the basalts . These rocks have also a positive qz , which is also a feature by which they differ from the basalts . Although it is difficult to place them under one heading into a classi ...
Страница 84
... also than the second series of magmatites ( hypabyssal plutonites north - west of Bor ) . ― These plutonites with skarn could have been cut by erosion only after their upheaval , that is after a strong tectonic phase , after which phase ...
... also than the second series of magmatites ( hypabyssal plutonites north - west of Bor ) . ― These plutonites with skarn could have been cut by erosion only after their upheaval , that is after a strong tectonic phase , after which phase ...
Страница 90
... also been stated earlier , the Cu - mineralization at Bor was deposited along a fault which can also occur in an intermediate intrusive ( quartz diorite , granodiorite , Marić , 1948 , monconite , Majer 1953 , Cissarz , 1956 ) as well ...
... also been stated earlier , the Cu - mineralization at Bor was deposited along a fault which can also occur in an intermediate intrusive ( quartz diorite , granodiorite , Marić , 1948 , monconite , Majer 1953 , Cissarz , 1956 ) as well ...
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Чести термини и фразе
амфибола анде андезитима Апатит Београд биотит биотитски амфиболски андезит биотитског амфиболског боје Борске Реке Брестовачке Бање бреча Бугарској вапнени већ више вјеројатно врло вулканита вулканских гдје Геологије дакле дацит дијелу дио дневног раскопа епидот Ерозија еруптивне стијене Жујовић затим Злота између има источној Србији истраживања их калцита Кварц кварца Клар клорит конгломерат конгломерата лабрадор Магма магматита магме магми магнетита међу међутим минерала мјестимице мјестимично можемо налази налазимо негдје области Тимочког базена овдје основи пелита пирит пироксена плагиокласа плутонита подручју Бора према Рутил саставу сенона серија сл Србији стијенама стијене тако такођер тимоцит треба ужем подручју ужој околини Бора фелдспата фенокристала Чока Чока Дулкан Чоке Чурули amphibole andesite biotite-amphibole andesite Bor conglomerate Borska Rijeka river calcareous Clar Čoka Dulkan composition dacite eastern Serbia facies find found groundmass igneous rocks later magma narrower region older open pit pelites phenocrysts plagioclase quartz diorite region of Bor rock Senonian strata timocit tuffs volcanic volcanites