Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Frederick J. Kuellmer"'
Autor:
Frederick J. Kuellmer
Publikováno v:
The Journal of Geology. 67:648-660
With the use of well-established relations between integrated intensities, integral breadths, and composition, a method is outlined by means of which it appears possible to determine the relative structural states of many perthitic alkali feldspars w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6b4ffb0b4b6d39057023aa7240380275
https://doi.org/10.1086/626623
https://doi.org/10.1086/626623
Autor:
Frederick J. Kuellmer
Publikováno v:
The Journal of Geology. 66:151-162
Near Hillsboro, New Mexico, a funnel-shaped quartz monzonite porphyry, containing large orthoclase cryptoperthite phenocrysts, intrudes early Tertiary (?) andesitic rocks. X-ray studies and analyses of these feldspars show that the (201) intensity ra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fe4f4bc3f12e26d0a7fe1b974a089d96
https://doi.org/10.1086/626491
https://doi.org/10.1086/626491
Publikováno v:
Southwestern New Mexico II.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2172c70bffba87cbed489d096356fda5
https://doi.org/10.56577/ffc-16.31
https://doi.org/10.56577/ffc-16.31
Autor:
Frederick J. Kuellmer
Granite, graywackes, and metadiabase, presumably Precambrian in age, are found only in small isolated areas within the mapped region.An aggregate thickness of 2,400 ft of sediments, representing a part of each Paleozoic period, overlies the Precambri
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::428659f8e0369bdd5d38095943140e41
https://doi.org/10.58799/b-33
https://doi.org/10.58799/b-33
Publikováno v:
South-central New Mexico.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::66776ab71f00743021aae2fa93cc7195
https://doi.org/10.56577/ffc-6.92
https://doi.org/10.56577/ffc-6.92