Zobrazeno 1 - 10
of 23
pro vyhledávání: '"Triassic dolomites"'
Publikováno v:
Fractal and Fractional, Vol 7, Iss 9, p 676 (2023)
Fractured aquifers, especially dolomites, are important hydrocarbon reservoirs and sources of thermal and groundwater in many parts of the world, especially in the Alpine-Dinaric-Carpathian region. The most dominant porosity type is fracture porosity
Externí odkaz:
https://doaj.org/article/bd9a72b33f774b93966da910e8a70f51
Publikováno v:
Rudarsko-geološko-naftni Zbornik, Vol 32, Iss 3, Pp 1-13 (2017)
This paper presents results of fractal analysis of fracture systems in upper Triassic dolomites in Žumberak Mountain, Croatia. Mechanical rock characteristics together with structural and diagenetic processes results with fracture systems that can b
Externí odkaz:
https://doaj.org/article/2dca9ac885e942cd8b0902080c26eb50
Akademický článek
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Autor:
Branko Sokač, Tonći Grgasović
Publikováno v:
Geologia Croatica, Vol 48, Iss 1, Pp 1-7 (2010)
Dissocladella bystrickyi n.sp. occurs in early diagenetic Upper Triassic dolomites, that were deposited in tidal flat and tidal channel environments in the carbonate platform interior. The new alga, assigned to the genus Dissocladella, is characteriz
Externí odkaz:
https://doaj.org/article/d151c0e7921d4ee9a02b9671d4240c0e
Autor:
Ivanić, Lara-Beatta
Geotermalna energija je energija sadržana u Zemljinoj unutrašnjosti. Hidrotermalni sustavi se razvijaju na mjestima gdje meteorska voda, procjeđivanjem kroz tektonske pukotine, dolazi u kontakt s izvorom topline te se konvekcijskim strujanjima vra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3908::6477e03b0a7e4101cf0bacb8b7af44f0
https://repozitorij.pmf.unizg.hr/islandora/object/pmf:8469
https://repozitorij.pmf.unizg.hr/islandora/object/pmf:8469
Autor:
Pavičić, Ivica
Pukotinska poroznost tektonskog porijekla najčešći je oblik poroznosti u dolomitima, dok se u manjoj mjeri pojavljuju taložna i dijagenetska poroznost. Pukotinska proznost pojavljuje se u rasponu mjerila od mikroskopskog do regionalnog. Provedeni
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3997::77ed2f0fd5dcf314be5d499061fedf1b
https://urn.nsk.hr/urn:nbn:hr:169:141347
https://urn.nsk.hr/urn:nbn:hr:169:141347
Autor:
Sokač, Branko, Grgasović, Tonći
Publikováno v:
Geologia Croatica, Vol 48, Iss 1, Pp 1-7 (2010)
Geologia Croatica
Volume 48
Issue 1
Geologia Croatica
Volume 48
Issue 1
Dissocladella bystrickyi n.sp. occurs in early diagenetic Upper Triassic dolomites, that were deposited in tidal flat and tidal channel environments in the carbonate platform interior. The new alga, assigned to the genus Dissocladella, is characteriz
During the Late Triassic the “Carnian Pluvial Event”, a global episode of climate change that involved increased rainfall and possibly global warming, a major crisis for carbonate producers is observed. In the western Tethys, the change in carbon
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::b580b3c5455f06227e1d037dbd314f63
http://hdl.handle.net/11368/2967050
http://hdl.handle.net/11368/2967050
In the late Carnian (Late Triassic), a carbonate-clastic depositional system including a distal alluvial plain, flood basin and sabkha, tidal flat and shallow carbonate lagoon was established in the Dolomites (Northern Italy). The flood basin was a m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9a73e51372f56ed941d9dd60f01fbe17
http://hdl.handle.net/11577/3156048
http://hdl.handle.net/11577/3156048