Zobrazeno 1 - 10
of 262
pro vyhledávání: '"N.T., Arndt"'
Autor:
Schuiling, R.D.
Publikováno v:
Earth-Science Reviews, 20(2), 180. Elsevier
The discovery of komatiites as a new class of rocks, was exciting. Komatiites are a key to our understanding of volcanism, tectonism and thermal regime in Archean times.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::d4299e6445fa685e60d95ea11145c339
https://dspace.library.uu.nl/handle/1874/24398
https://dspace.library.uu.nl/handle/1874/24398
Publikováno v:
Earth-Science Reviews. 20(2):180
The discovery of komatiites as a new class of rocks, was exciting. Komatiites are a key to our understanding of volcanism, tectonism and thermal regime in Archean times.
Autor:
Hofman, Paul1,2,3 (AUTHOR) hofman.p@chu-nice.fr
Publikováno v:
Cancers. Oct2024, Vol. 16 Issue 19, p3340. 17p.
Autor:
C.M. Lesher, N.T. Arndt
It is easy to explain roughly what a komatiite is, but difficult to give a rigorous definition. The simple definition, as given by Arndt and Nisbet in 1982, is that komatiite is an ultramafic volcanic rock. A limit of 18% MgO separates komatiites fro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::70de9bf1fb2b6e8420e8341909d0d584
https://doi.org/10.1016/b0-12-369396-9/00297-5
https://doi.org/10.1016/b0-12-369396-9/00297-5
Autor:
Bruneton, M., H.A., Pedersen, Farra, V., N.T., Arndt, Vacher, P., Achauer, U., Alinaghi, A., Ansorge, J., Bock, G., Friederich, W., Grad, M., Guterch, A., Heikkinen, P., S.E., Hjelt, T.L., Hyvönen, J.P., Ikonen, Kissling, E., Korja, A., Kozlovskaya, E., M.V., Nevsky, Paulssen, H., N.I., Pavlenkova, Plomerovà, J., Raita, T., O.Y., Riznichenko, R.G., Roberts, Sandoval, S., I.A., Sanina, N.V., Sharov, Z.H., Shomali, Tiikkainen, J., Wielandt, E., Wilegalla, K., Yliniemi, J., Y.G., Yurov
Publikováno v:
Journal of Geophysical Research
Journal of Geophysical Research, American Geophysical Union, 2004, 109 (B10), pp.B10303. ⟨10.1029/2003JB002947⟩
Journal of Geophysical Research, American Geophysical Union, 2004, 109 (B10), pp.B10303. ⟨10.1029/2003JB002947⟩
International audience
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::bc3dc67d31689b2069c9b681b9c3dca7
https://hal.archives-ouvertes.fr/hal-00118054/file/2003JB002947.pdf
https://hal.archives-ouvertes.fr/hal-00118054/file/2003JB002947.pdf
Autor:
Bruneton, M., H.A., Pedersen, Vacher, P., I.T., Kukkonen, N.T., Arndt, Funke, S., Friederich, W., Farra, V., Group, Svekalapko
Publikováno v:
Earth and Planetary Science Letters
Earth and Planetary Science Letters, Elsevier, 2004, 226, pp.41-52
Earth and Planetary Science Letters, Elsevier, 2004, 226, pp.41-52
International audience
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::3435dd4433dacc5bada5628c13fe4623
https://hal.archives-ouvertes.fr/hal-00118055
https://hal.archives-ouvertes.fr/hal-00118055
Autor:
N.T. Arndt
Publikováno v:
Lithos. :148-149
Autor:
N.T. Arndt
Publisher Summary Twenty-five years have passed since komatiites were first recognized in South Africa by Richard and Morris Viljoen and the existence of ultramafic volcanic rocks is now generally accepted. Occurrences are known in all continents exc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ada40f71cc9ad15d0d6e7d9a381f4e65
https://doi.org/10.1016/s0166-2635(08)70219-6
https://doi.org/10.1016/s0166-2635(08)70219-6
Publikováno v:
Chemical Geology. 120:iii-iv