Zobrazeno 1 - 10
of 16
pro vyhledávání: '"Jouni Vuollo"'
Autor:
Fang-Fang Guo, Wolfgang D. Maier, Jussi S. Heinonen, Eero Hanski, Jouni Vuollo, Sarah-Jane Barnes, Yann Lahaye, Hannu Huhma, Shenghong Yang
Publikováno v:
Lithos. :107206
Autor:
Richard E. Ernst, Jouni Vuollo, Kevin R. Chamberlain, S. C. Davey, Hannu Huhma, W Bleeker, Brian Cousens, Sandra L. Kamo
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
Jouni Vuollo, James Passmore, Daniel Cassard, Oliver Raymond, Mark Rattenbury, Michael Sexton
EarthResourceML (http://www.earthresourceml.org) is the international data model and standard for mineral resources data. EarthResourceML (ERML) was initially developed for the Australian Chief Government Geologists Committee (CGGC) but is now under
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cae3a38cb6e965bdb628ffec9080ed2d
https://doi.org/10.1002/essoar.10500202.1
https://doi.org/10.1002/essoar.10500202.1
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 82, Iss 1, Pp 31-62 (2010)
Using the SIMS, ID-TIMS and Sm-Nd isotopic methods and the electron microprobe, we have studied several differentiated mafic intrusions of the c. 2.2 Ga gabbro-wehrlite association (GWA) from four Paleoproterozoic schist belts and the Archean Kuhmo G
Publikováno v:
Precambrian Research. 92:89-116
Palaeoproterozoic mafic igneous rocks (2500–2440 Ma) are exposed in the form of layered intrusions, dykes, and volcanic rocks in the southern Canadian Shield and the Fennoscandian Shield. Both igneous events were associated with episodes of contine
Publikováno v:
Lithos. 36:15-27
Chromites from the ultramafic rocks of the early Proterozoic Outokumpu-Jormua Ophiolite Belt were found to possess textural and Cr (Cr + Al) and Mg (Mg + Fe 2+ ) ratios that resemble those described in Mesozoic ophiolite complexes. Chromites of cumul
Autor:
Jouni Vuollo, Elias Ekdahl, Jussi P. Liipo, Lauri Pekkarinen, Tauno A. Piirainen, Vesa Nykänen, Ilkka Tuokko
Publikováno v:
Economic Geology. 90:445-452
Publikováno v:
Precambrian Research. 70:45-65
The Palaeoproterozoic sedimentary cover of the Archaean basement complex in the Fennoscandian Shield is intruded by several stages of mantle-derived magmas. The 2.1 Ga Fe-tholeiitic magmatism, which is characterized by hypabyssal intrusions, dykes an
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 66, Iss 1, Pp 3-18 (1994)
Investigations into chromite compositions in Archaean ultramafic rocks are rare. Most Archaean ultramafic rocks have undergone a multi-stage history of deformation and metamorphism, and therefore fresh primary chromite is rarely preserved. The preser