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                                       Details for article 12 of 14 found articles
 
 
  Quaternary gabbro-anorthosites as effusives in Kamchatka
 
 
Title: Quaternary gabbro-anorthosites as effusives in Kamchatka
Author: Yermakov, V. A.
Petrov, V. S.
Gusakova, N. R.
Appeared in: International geology review
Paging: Volume 19 (1977) nr. 1 pages 75-79
Year: 1977-01
Contents: Holocrystalline gabbro-anorthosites and anorthosites have been found in the thick interformational veins of the upper portions of the Pliocene-Quaternary Nikolka volcano in Kamchatka. The gabbro-anorthosites contain a marked amount of K-feldspar, and on the basis of their chemistry, they have been assigned to the tephrite-basalts. They are identical to the megaplagiophyre basalts, which are widely distributed in the Central Kamchatka depression. It has been suggested that the magma of subalkaline gabbro-anorthosites occurred in signifcant depths at the base of the crust during emanation differentiation of a saturated tholeiite. Further fractionation of this magma could have led to the formation of autonomous anorthosites and alkaline gabbroids associated with them in natural assemblages. —Authors.
Publisher: Taylor & Francis
Source file: Elektronische Wetenschappelijke Tijdschriften
 
 

                             Details for article 12 of 14 found articles
 
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