Zobrazeno 1 - 10
of 381
pro vyhledávání: '"Intraclasts"'
Publikováno v:
地质科技通报, Vol 40, Iss 6, Pp 140-150 (2021)
There is shallow sea sandy debris flow in Ying Ⅱ Member in Dongfang 1-1 Gas Field, Yinggehai Basin.Based on the detailed description of cores, combined with well logs, seismic section, geochemical experiments and the research progress of gravity fl
Externí odkaz:
https://doaj.org/article/472a207b2a7e4016833af18e6e4dbd93
Publikováno v:
Известия высших учебных заведений: Геология и разведка, Vol 0, Iss 3, Pp 69-81 (2021)
Background. In this article, we investigate an outcrop of the Lower Jurassic limestones of the Eskiorda suite located on the northern slope of the Bodrak River basin in the south-western Crimea.Aim. The outcrop under study is mentioned in the majorit
Publikováno v:
Sedimentology. 69:199-218
Three Holocene tufas from Gran Canaria volcanic island were studied with the aim of deciphering their sedimentary evolution through space and time. Las Temisas tufa (south-eastern arid part of the island) is dominantly composed of oncoids, intraclast
Publikováno v:
Sedimentology. 68:3385-3404
Early Triassic temperatures were some of the hottest of the Phanerozoic, sea-surface temperatures approached 40°C, with profound consequences for both the sedimentology and faunal distributions in the oceans. However, the impact of these temperature
Publikováno v:
Geologia Croatica
Volume 74
Issue 2
Volume 74
Issue 2
Istrian Flysch was deposited during the Eocene in the Dinaric foredeep and is composed of hemipelagic marls and various gravity flow deposits. The latter are predominantly 5-40 cm thick turbidites, developed mostly as laminated and cross-rippled sand
Publikováno v:
Iraqi Geological Journal, Vol 54, Iss 1E, Pp 29-42 (2021)
The studied section is located in the core of the Gara Anticline, about 12 km southeast of Amedi Town. The Baluti Formation is generally composed of grey and green shale, calcareous, dolostone with intercalations of thinly bedded dolostones, dolomiti
Publikováno v:
Journal of Iberian Geology. 47:501-534
The Toarcian–Aalenian(?) Cabo Carvoeiro Formation in the Lusitanian Basin (LB), Portugal, is characterized by a succession of mixed carbonate–siliciclastic sediments deposited under the influence of an active horst-graben system caused by the pro
Autor:
Guilherme Furlan Chinelatto, Alexandre Campane Vidal, João Paulo da Ponte Souza, Mateus Basso, Aline Maria Poças Belila
Publikováno v:
International Journal of Earth Sciences. 110:2573-2595
Lacustrine carbonate deposits mark the rift-sag sedimentation stage of the so-called pre-salt section of the Campos and Santos Basins, in the Southeast Brazilian continental shelf. These salt-sealed carbonate reservoirs form deep-water, giant and pro
Publikováno v:
AAPG Bulletin. 104:1593-1624
Grain assemblages in the organic-rich Cline shale in the Midland Basin are dominated by components of extrabasinal derivation (11.4 to 98.5 vol. %; average volume: 82.6%). Major extrabasinal components include K-rich clay minerals, detrital quartz, a
Publikováno v:
Geologia Croatica
Volume 73
Issue 2
Volume 73
Issue 2
Maastrichtian to Palaeocene pelagic carbonates on the central Adriatic island of Svetac (Sveti Andrija) are the only outcrops reported to date that document pelagic deposition during the Cretaceous–Palaeogene (K–Pg) transition within the Adriatic