Zobrazeno 1 - 10
of 12
pro vyhledávání: '"J. C. Rucklidge"'
Publikováno v:
AIP Conference Proceedings.
Accelerator mass spectrometry has been applied, in a very few laboratories, to the in-situ analysis of trace elements in solids such as metals, semiconductors and minerals. The latter have largely been electrically-conducting phases with minimum grai
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ed269db17cb9b7261cce72d86493f9bb
https://doi.org/10.1063/1.59203
https://doi.org/10.1063/1.59203
Autor:
J. C. Rucklidge
Publikováno v:
X-Ray Spectrometry. 7:57-62
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9dccfe8f7119c5d4a6b8e57e8e08b454
https://doi.org/10.1002/xrs.1300070204
https://doi.org/10.1002/xrs.1300070204
Publikováno v:
Mineralogical Magazine. 45:211-218
Whole-rock, minor element, rare earth, and electron microprobe data are presented for basaltic lavas from the western Kangerdlugssuaq area of East Green- land. Samples were obtained from Professor W. A. Deer's 1936 collection at Triangular Nunataks a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::88a3bbee9a0c3658ad9927c53534305b
https://doi.org/10.1180/minmag.1982.045.337.24
https://doi.org/10.1180/minmag.1982.045.337.24
Autor:
G. C. Wilson, J. C. Rucklidge
Publikováno v:
Mineralogy and Petrology. 36:219-239
This paper describes mineralogical and geological aspects of the Owl Creek and Hoyle Pond gold mines, located in Archean metasediments and metavolcanics in the Abitibi greenstone belt in northern Ontario, Canada. The occurrence of “invisible gold
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::14561063b474076b212969e078230e0c
https://doi.org/10.1007/bf01163261
https://doi.org/10.1007/bf01163261
Publikováno v:
Canadian Journal of Earth Sciences. 8:144-149
The degree of preferred orientation of hornblende in two boudinage structures is analyzed by means of an X-ray texture goniometer. Relative values of reflected intensity for {110} are plotted on the stereographic net, and contoured at convenient inte
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3fd692eed23dda6b005f73a5c8579c50
https://doi.org/10.1139/e71-010
https://doi.org/10.1139/e71-010
Publikováno v:
Economic Geology. 62:502-516
The Lamaque and Sigma ore zones are composed of a multiplicity of gold-bearing quartz veins extending vertically to depths greater than 4,000 feet. The mines are about 2,500 feet apart horizontally and they are separated by a steeply dipping fault zo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a8ab1e16692c16804e7ffe9b54f42c2b
https://doi.org/10.2113/gsecongeo.62.4.502
https://doi.org/10.2113/gsecongeo.62.4.502
Autor:
J. Zussman, J. C. Rucklidge
Publikováno v:
Acta Crystallographica. 19:381-389
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::31a5213044986242ab9c5b54c1cce5ec
https://doi.org/10.1107/s0365110x65003493
https://doi.org/10.1107/s0365110x65003493
Publikováno v:
Canadian Journal of Earth Sciences. 6:340-344
In a search for Tertiary dikes, rocks were collected along part of the east coast of Labrador. K–Ar age determinations on some of these rocks suggest that the Grenville Front passes out to sea along the north side of Groswater Bay.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a1e54ef7e6f01ef30cdd0987f1dd6eef
https://doi.org/10.1139/e69-030
https://doi.org/10.1139/e69-030
Autor:
J. C. Rucklidge, W. A. Elders
Publikováno v:
The Journal of Geology. 77:240-244
Excellent exposures along the coast of Labrador for 150 km. reveal a consistent pattern of thick gabbro sheets overlying migmatic granite gneisses. The relationship between the two rocks is complex, and in many places each appears to have intruded th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d6867b0df3f661582dbbad60f4b50171
https://doi.org/10.1086/627424
https://doi.org/10.1086/627424
Publikováno v:
Nature. 212:603-604
DURING the summer of 1965 the Oxford University Expedition to East Greenland visited the north-eastern section of the extensive area of Tertiary lavas which stretches northwards from Kangerdlugssuaq to the Scoresby Sund fjord system. This communicati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::20a0743202cb0c52f83e5d927238c8a1
https://doi.org/10.1038/212603a0
https://doi.org/10.1038/212603a0