Zobrazeno 1 - 10
of 20
pro vyhledávání: '"Thomas O. Reimer"'
Autor:
David J. Mossman, Thomas O. Reimer
Publikováno v:
Economic Geology. 85:337-343
Recent revisionist criticism of the modified placer theory of the origin of the Witwatersrand ores is singularly unconvincing. In response to that criticism it is shown that the so-called enigma of the sulfidation of black sands is a myth; sulfide as
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b09a2ac10ed14a3e622e76f90dd126da
https://doi.org/10.2113/gsecongeo.85.2.337
https://doi.org/10.2113/gsecongeo.85.2.337
Autor:
Thomas O. Reimer, David J. Mossman
Publikováno v:
Mineralium Deposita. 46:837-838
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::da1c83b8e7c4a319705933260d770c41
https://doi.org/10.1007/s00126-011-0369-0
https://doi.org/10.1007/s00126-011-0369-0
Autor:
Thomas O. Reimer
Publikováno v:
Early Organic Evolution ISBN: 9783642768866
Extensive beds of carbonaceous shale occur within a thick sequence of Lower Proterozoic dolostone, the lower Transvaal Supergroup of South Africa. The shale contains such high concentrations of A12O3 (21.9%) and K2O (6.5%) that it is compositionally
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2d0f60bc9d2cbb86c512f959a04441d8
https://doi.org/10.1007/978-3-642-76884-2_8
https://doi.org/10.1007/978-3-642-76884-2_8
Autor:
Thomas O. Reimer
Publikováno v:
The Canadian Mineralogist. 38:1492-1492
This is the ultimate hard-cover book in the truest sense of the word: a total of 95 pages solidly bound between two A4-sized vinyl floor tiles. You even get hints how to the handle the book. For example, the author warns that in very cold climates, t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::00102b5d7ceb3c79c841bb27671beb0d
https://doi.org/10.2113/gscanmin.38.6.1492
https://doi.org/10.2113/gscanmin.38.6.1492
Autor:
Thomas O. Reimer
Publikováno v:
Economic Geology. 85:1949-1950
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7407c591a2e252eae044e213da509a5c
https://doi.org/10.2113/gsecongeo.85.8.1949
https://doi.org/10.2113/gsecongeo.85.8.1949
Publikováno v:
Geology. 19:536
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3a3b18db0b56f77b6aec6752b3506a16
https://doi.org/10.1130/0091-7613(1991)019<0536:caroso>2.3.co
https://doi.org/10.1130/0091-7613(1991)019<0536:caroso>2.3.co
Autor:
Thomas O. Reimer, David J. Mossman
Publikováno v:
Geology. 18:426
Reassessment of the nature and distribution of iron-titanium oxide minerals vs. pyrite in several South African Archean arenaceous sequences and conglomerates shows that in rocks of the Swaziland, Pongola, and Witwatersrand Supergroups, (1) pyrite of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::08eb8374897ae026e2117a88a7eb67ca
https://doi.org/10.1130/0091-7613(1990)018<0426:sowbsf>2.3.co
https://doi.org/10.1130/0091-7613(1990)018<0426:sowbsf>2.3.co
Autor:
Thomas O. Reimer
Publikováno v:
Precambrian Research. 26:223-234
Data on the occurrence of graphite and other highly reconstituted carbonaceous matter as potential traces of carbon originally derived from organic matter are compiled from Precambrian rocks of Namibia, Botswana, South Africa, and Zimbabwe. While car
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::96f67e2d19580d027773dcf310548131
https://doi.org/10.1016/0301-9268(84)90002-0
https://doi.org/10.1016/0301-9268(84)90002-0
Publikováno v:
Precambrian Research. 29:383-404
Pebbles of potassic granitoids and metamorphites constitute up to 5% of the basal conglomerate of the Moodies Group in a ratio of 2 : 1. The granitoid pebbles frequently show micrographic quartz–feldspar intergrowth, whereas the metamorphites—of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f8c06e207f262bc24e401e87a42c23bd
https://doi.org/10.1016/0301-9268(85)90044-0
https://doi.org/10.1016/0301-9268(85)90044-0
Autor:
Thomas O. Reimer
Publikováno v:
Journal of the Geological Society. 141:263-271
Present models of the derivation of the gold in the Witwatersrand conglomerates of South Africa as detrital grains directly from primary deposits in a source area consisting mainly of Archaean schist belts meets with a volume problem. Witwatersrand d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::19945462616f597b2bb673b78de6b1de
https://doi.org/10.1144/gsjgs.141.2.0263
https://doi.org/10.1144/gsjgs.141.2.0263