Zobrazeno 1 - 10
of 24
pro vyhledávání: '"J. C. Hunziker"'
Publikováno v:
Deep Structure of the Swiss Alps ISBN: 9783034899055
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f1dab70457f755132c9e8a85a61ca99f
https://doi.org/10.1007/978-3-0348-9098-4_20
https://doi.org/10.1007/978-3-0348-9098-4_20
Publikováno v:
Deep Structure of the Swiss Alps ISBN: 9783034899055
Deep Structure of the Swiss Alps
Deep Structure of the Swiss Alps
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::88d7e80aad706f9a722775a35b566e58
https://doi.org/10.1007/978-3-0348-9098-4_16
https://doi.org/10.1007/978-3-0348-9098-4_16
Autor:
J. C. Hunziker
Publikováno v:
Geological Society, London, Special Publications. 19:221-227
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c03843ce97f930da038170a443c432c7
https://doi.org/10.1144/gsl.sp.1986.019.01.12
https://doi.org/10.1144/gsl.sp.1986.019.01.12
Publikováno v:
Geological Society, London, Special Publications. 45:353-367
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::49a17795469c5cd243e0dc141d72724c
https://doi.org/10.1144/gsl.sp.1989.045.01.20
https://doi.org/10.1144/gsl.sp.1989.045.01.20
Publikováno v:
Contributions to Mineralogy and Petrology. 97:31-42
The Ivrea zone represents a tilted cross section through deep continental crust. Sm-Nd isotopic data for peridotites from Baldissero and Balmuccia and for a suite of gabbros from the mafic formation adjacent to the Balmuccia peridotite provide eviden
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f4ee5b0200e5b5cf88928ae9d0698842
https://doi.org/10.1007/bf00375212
https://doi.org/10.1007/bf00375212
Publikováno v:
Geologische Rundschau. 67:243-252
Der Nevado Coropuna (6400 m) ist der groste und machtigste Vulkan Perus. Er erhebt sich 150 km NW von Arequipa und 110 km von der pazifischen Kuste uber den Westabfall der Anden. Ergebnisse geologischer, petrographischer und geochronologischer Unters
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::13827891492eddb8ab802085d202c6bd
https://doi.org/10.1007/bf01803264
https://doi.org/10.1007/bf01803264
Publikováno v:
Journal of Structural Geology. 8:781-798
Paleozoic to Oligocene metasedimentary rocks present in the Alpi Apuane region of the Northern Apennines, Italy, have been sequentially deformed during a Tertiary progressive deformation. In an attempt to date the individual deformation episodes, ove
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e9289fe99ffe98d10ec007f35d90c47a
https://doi.org/10.1016/0191-8141(86)90025-8
https://doi.org/10.1016/0191-8141(86)90025-8
Publikováno v:
Journal of the Geological Society. 135:481-497
Glauconite is abundant in many Palaeogene rocks and its contained potassium can be used for radiometric dating. The methodology of this dating is described and sources of error and uncertainty are examined. Age determinations are presented on thirty-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ff90d7a9ba80c4ebd54749064008f007
https://doi.org/10.1144/gsjgs.135.5.0481
https://doi.org/10.1144/gsjgs.135.5.0481
Publikováno v:
Contributions to Mineralogy and Petrology. 83:185-197
Some 150 white K-micas from the Central Alps were analysed for their polymorph and phengite content.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::57bf70bfa36335612a807f49a50f19e3
https://doi.org/10.1007/bf00373092
https://doi.org/10.1007/bf00373092
Publikováno v:
Geologische Rundschau. 67:719-742
Along the southern margin of the Damara orogen age and degree of metamorphism were determined by means of K/Ar dating and illite crystallinity. The investigations include the following units: The metamorphism of the Naukluft nappes as well as the und
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::929f57852450fc68a900c9d869aa3bd9
https://doi.org/10.1007/bf01802814
https://doi.org/10.1007/bf01802814