Results 61 to 70 of about 108,116 (201)

Facies development during late Early-Middle Cambrian (Tayan Member, Burj Formation) transgression in the Dead Sea Rift valley, Jordan

open access: yesCarnets de Géologie, 2007
The transgressive Tayan Member of the upper Lower to Middle Cambrian Burj Formation (Jordan) has been investigated in several localities of the Dead Sea Rift valley, Jordan.
Elicki Olaf
doaj  

Localization and further extraction of residual recoverable oil reserves in low-permeability sandstone reservoirs with chaotic oblique layering in a late-stage field: a case study of the Achimov sequence

open access: yesИзвестия высших учебных заведений: Нефть и газ
Achimov sequence is characterized by high heterogeneity and low reservoir properties. Development of Achimov sequence occurs using horizontal wells with multistage hydraulic fracturing.
T. K. Apasov, A. G. Kudiiarov
doaj   +1 more source

Map of work units based on cluster analysis for similar management decision (C11: facies 4,6,8,9,16; C2: facies 1,5,7,11,15; C121: facies 12,13; C1222; facies 2; C1221: facies 3,10,14,17).

open access: yes, 2019
Map of work units based on cluster analysis for similar management decision (C11: facies 4,6,8,9,16; C2: facies 1,5,7,11,15; C121: facies 12,13; C1222; facies 2; C1221: facies 3,10,14,17).
Hassan Khosravi (8150787)   +4 more
core   +1 more source

Facies, development and interpretation of sedimentary environment of the uranium-bearing Brebovnica Member of the Val Gardena Formation in the Žirovski vrh area, W Slovenia

open access: yesGeologija, 2002
The Brebovnica Member, bearing considerable grades of uranium ore, is the most important member of the Val Gardena Formation. Rocks were subdivided according to grain size, sedimentary structures and composition to conglomerate, sandstone, mudstone and ...
Dragomir Skaberne
doaj  

Carbonate Facies and Sedimentation of the Klapanunggal Formation in Cibinong, West Java

open access: yesIndonesian Journal on Geoscience, 2014
DOI:10.17014/ijog.v1i3.196The limestone of Klapanunggal Formation is well exposed in the area of Cibinong and its surrounding,West Java. Detailed Observation of carbonate rock has been conducted in this area and aims to studythe carbonate facies and its ...
Praptisih Praptisih, Kamtono Kamtono
doaj   +1 more source

Mauskopf facies [PDF]

open access: yesBMJ Case Reports, 2013
Deepak, Sundriyal   +3 more
openaire   +2 more sources

Facies and paleoenvironmental reconstruction of Early–Middle Miocene deposits in the north-west of the Zagros Basin, Iran

open access: yesGeologica Carpathica, 2019
Facies analysis and paleoenvironmental reconstruction of the Burdigalian to Langhian Asmari Formation, outcropping in the Khorram Abad Anticline, in the north-west of the Zagros Basin allow us to interpret the carbonate ramp history during the Early ...
Roozpeykar Asghar   +3 more
doaj   +1 more source

About the structure of the Kama-Kinel trough system

open access: yesИзвестия высших учебных заведений: Геология и разведка, 2019
Kama-Kinel Trough System (KKTS) — the structure formed in the Frasnian of the Late Devonian in the vast territory of the Volga-Ural province, is distinguished by the Upper Devonian — Lower Carboniferous deposits.
E. N. Gorozhanina   +3 more
doaj   +1 more source

Facies-based rock properties characterization for CO2 sequestration: GSWA Harvey 1 well, Western Australia

open access: yes, 2014
GSWA Harvey 1 was drilled as part of the South West CO2 Geosequestration Hub carbon capture and storage project (South West Hub) to evaluate storage volume, injectivity potential and carbon dioxide retention capacity in the south-western Perth Basin. Six
Nicholas Timms (10126988)   +6 more
core  

Permian Carbonates in the Venezuelan Andes [PDF]

open access: yes, 2012
In northern South America, Upper Palaeozoic strata were deposited extensively over peri-cratonic areas associated with restricted seas located between Laurentia and Gondwana, in equatorial Pangea. In many places the successions are rarely exposed, and so
Laya-Pereira, Juan Carlos   +1 more
core  

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