Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Ron Goldbery"'
Autor:
M. Beyth, Ron Goldbery
Publikováno v:
Sedimentology. 31:575-594
Field and laboratory investigations of the Triassic Budra Formation of Wadi Budra, south-west Sinai, have demonstrated the existence of surface pedogenic laterites developed within‘overbank facies’of fluviatile sediments during times of hiatus. T
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::58ebe085e7c586db23ff398a867433bb
https://doi.org/10.1111/j.1365-3091.1984.tb01821.x
https://doi.org/10.1111/j.1365-3091.1984.tb01821.x
Autor:
Ron Goldbery, F. C. Loughnan
Publikováno v:
Sedimentology. 24:565-579
Dawsonite, alumohydrocalcite, nordstrandite, gorceixite and calcite are associated in marine strata of the Permian Shoalhaven Group of the Sydney Basin, south-eastern Australia. The assemblages were apparently of late syngenetic or epigenetic develop
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aac672d4f3458140a12697d5730b4856
https://doi.org/10.1111/j.1365-3091.1977.tb00139.x
https://doi.org/10.1111/j.1365-3091.1977.tb00139.x
Autor:
Ron Goldbery
Publikováno v:
Sedimentary Geology. 31:119-140
A sequence of palaeosols developed on exposed overbank sediments of successive alluvial cycles of the Lower Jurassic “Laterite Derivative Facies” (LDF) at Makhtesh Ramon, contains well-developed, penecontemporaneous soil microrelief structures. T
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::24d8ac8e8d9378caea00908d32ae2255
https://doi.org/10.1016/0037-0738(82)90034-3
https://doi.org/10.1016/0037-0738(82)90034-3
Publikováno v:
Sedimentary Geology. 35:105-152
The Lower Jurassic section at Makhtesh Ramon, in the northeastern Negev of Israel, comprises a sequence of fluviatile sediments of laterite composition. Post-depositional chemical weathering has resulted in marked facies changes whereby the clastic s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::83227f0431f7abb187bbcf272d16250a
https://doi.org/10.1016/0037-0738(83)90047-7
https://doi.org/10.1016/0037-0738(83)90047-7
Autor:
Ron Goldbery
Publikováno v:
Sedimentology. 26:229-251
Petrographical and mineralogical studies of the Lower Jurassic sequence exposed at Makhtesh Ramon, have shown the domination of a lateritic suite of epiclastic sediments of pisolite conglomerate and laterite arenite composition. Their subsequent modi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2664eabbe1488abec9a6c3e05176f93d
https://doi.org/10.1111/j.1365-3091.1979.tb00352.x
https://doi.org/10.1111/j.1365-3091.1979.tb00352.x
Autor:
Ron Goldbery
Publikováno v:
Sedimentology. 27:189-198
An early diagenetic non-hydrothermal deposit of Na-alunite [(Na,K)Al3(SO4)2(OH)6] is described from the Miocene Ras Maalab Group at Ras Sudar Sinai. The alunite is nodular and occurs along two horizons parallel to bedding. Displacive growth structure
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bc8f2f9259dc7895186463b9803c7755
https://doi.org/10.1111/j.1365-3091.1980.tb01169.x
https://doi.org/10.1111/j.1365-3091.1980.tb01169.x
Autor:
Ron Goldbery
Publikováno v:
SEPM Journal of Sedimentary Research. 49
Textural inversion occurs in a red bed horizon of the Lower Jurassic Ardon Formation at Makhtesh Ramon. This texture consists of highly spherical, well rounded very well-sorted, coarse quartz grains, dispersed within an argillaceous silty micrite. Th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::647663d641bc3045e426366b7208b982
https://doi.org/10.1306/212f786a-2b24-11d7-8648000102c1865d
https://doi.org/10.1306/212f786a-2b24-11d7-8648000102c1865d
Autor:
Ron Goldbery
Publikováno v:
SEPM Journal of Sedimentary Research. 50
The Pliocene Pleshet Formation was deposited in moderately high energy, nearshore environments dominated by upper shoreface and foreshore sediments, characterized by concentrations of heavy minerals and shell fragments, beach rock, shoreline conglome
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::10625c9a2d0ce96f9c02d5c858606b70
https://doi.org/10.1306/212f7b08-2b24-11d7-8648000102c1865d
https://doi.org/10.1306/212f7b08-2b24-11d7-8648000102c1865d
Autor:
Ron Goldbery
Publikováno v:
Geological Society of America Bulletin. 89:687
A newly discovered deposit of aluminum sulfate minerals within kaolinite claystones of the Middle Jurassic Inmar Formation at Makhtesh Ramon is described. The sulfate minerals as determined by X-ray diffraction, chemical analysis, and differential th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ac37173563fc53a34d36f88d2aaa52f3
https://doi.org/10.1130/0016-7606(1978)89<687:ednnij>2.0.co
https://doi.org/10.1130/0016-7606(1978)89<687:ednnij>2.0.co