Two contrasting petrotectonic domains in the Kokchetav megamelange (north Kazakhstan) : Difference in exhumation mechanisms of ultrahigh-pressure crustal rocks, or a result of subsequent deformation?
スポンサーリンク
概要
- 論文の詳細を見る
- 2000-09-01
著者
-
Smirnova L.
United Institute Of Geology Geophysics And Mineralogy Sb Of The Russian Academy Of Sciences
-
DOBRETSOV N.
United Institute of Geology, Geophysics and Mineralogy, Russian Academy of Sciences, Siberian Branch
-
SHATSKY V.
United Institute of Geology, Geophysics and Mineralogy, Russian Academy of Sciences, Siberian Branch
-
Shatsky V.
United Institute Of Geology Geophysics And Mineralogy Sb Of The Russian Academy Of Sciences
-
Shatsky V.
United Institute Of Geology Geophysics And Mineralogy Russian Academy Of Sciences Siberian Branch
-
Dobretsov N.
United Institute Of Geology Geophysics And Mineralogy Sb Of The Russian Academy Of Sciences
-
Dobretsov N.
United Institute Of Geology Geophysics And Mineralogy Russian Academy Of Sciences Siberian Branch
-
THEUNISSEN K.
Department of Geology and Mineralogy, Royal Museum for Central Africa
-
KORSAKOV A.
United Institute of Geology, Geophysics and Mineralogy, SB of the Russian Academy of Sciences
-
TRAVIN A.
United Institute of Geology, Geophysics and Mineralogy, SB of the Russian Academy of Sciences
-
BOVEN A.
Laboratory of Geochronology, Vrije Universiteit Brussel
-
Boven A.
Laboratory Of Geochronology Vrije Universiteit Brussel
-
Korsakov A.
United Institute Of Geology Geophysics And Mineralogy Sb Of The Russian Academy Of Sciences
-
Theunissen K.
Department Of Geology And Mineralogy Royal Museum For Central Africa
-
Travin A.
United Institute Of Geology Geophysics And Mineralogy Sb Of The Russian Academy Of Sciences
関連論文
- Geotectonic evolution of diamondiferous paragneisses, Kokchetav Complex, northern Kazakhstan : The geologic enigma of ultrahigh-pressure crustal rocks within a Paleozoic foldbelt
- Two contrasting petrotectonic domains in the Kokchetav megamelange (north Kazakhstan) : Difference in exhumation mechanisms of ultrahigh-pressure crustal rocks, or a result of subsequent deformation?