Zobrazeno 1 - 10
of 311
pro vyhledávání: '"S. Boya"'
Autor:
Kgaugelo S. Boya
Publikováno v:
HTS Teologiese Studies/Theological Studies, Vol 78, Iss 1, Pp e1-e7 (2022)
Traditionally, churches exist to fulfil the ‘great commission’, which is to preach the ‘good news’ to all believers. As the ‘great commission’ finds expression within the Church, numerical growth becomes inevitable. The latter puts pressu
Externí odkaz:
https://doaj.org/article/564ab5c357574b8e81e6c88a9d2e3021
Akademický článek
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Publikováno v:
Journal of the Geological Society. 176:1182-1190
We investigate how sedimentary systems respond to tectonic uplift during the last stages of infilling of a foreland basin. Massive conglomeratic deposits characterize the last stage of basin fill in the Jaca basin, the western portion of the South Py
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ec1fa1806b5e3a865c0d3d2d67f8a083
https://doi.org/10.1144/jgs2018-228
https://doi.org/10.1144/jgs2018-228
Thick shallow-marine successions associated with long-term transgressions are less well known than their thin, well-sorted counterparts, widely studied due to their potential to form good reservoirs. In these successions, particularly in storm-domina
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::02c6bfb83888acef3f1e619d7030eff9
https://doi.org/10.5194/egusphere-egu21-16005
https://doi.org/10.5194/egusphere-egu21-16005
Publikováno v:
SEDICI (UNLP)
Universidad Nacional de La Plata
instacron:UNLP
Universidad Nacional de La Plata
instacron:UNLP
Thick (>100 m-thick), highly bioturbated storm-influenced shallow-marine deposits are not frequent in the stratigraphic record, but they tend to be common in aggradational to retrogradational successions. Individual storm-event beds have typically lo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e3df644849219dc599ab9410b8ff0c65
http://sedici.unlp.edu.ar/handle/10915/129551
http://sedici.unlp.edu.ar/handle/10915/129551
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
The Eocene clastic systems of the Jaca foreland Basin (southern Pyrenees) allow us to identify changes in sediment composition through time. We provide new data on sediment composition and sources of the northern Jaca basin, whose stratigraphic evolu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d8e45e4b2df05be2070b5e6c942ba179
https://doi.org/10.1016/j.crte.2015.10.005
https://doi.org/10.1016/j.crte.2015.10.005
Supplementary material 3: Full detrital zircon U–Pb spectra from 0 Ma to 3500 Ma, displayed as kernel density estimators (KDE) and histograms (Vermeesch, 2012). Nonadaptive KDE bandwidth of 8 Ma, histogram bin width of 20 Ma.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1d653d6a0d8ca3c0e2295ba1278c54e9
Supplementary material 1: Extended Zircon U–Pb LA–ICP–MS methodology.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2c3c8e30aaf1d9fb0311484bbbb6865f
Akademický článek
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Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
In the northern Jaca basin (Southern Pyrenees), the replacement of deep-marine by terrestrial environments during the Eocene records a main drainage reorganization in the active Pyrenean pro-wedge, which leads to recycling of earlier foreland basin s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f47dad2db034ac22aeea0a12b3efe8a0
http://hdl.handle.net/10261/157189
http://hdl.handle.net/10261/157189