Russian Mineralogical Society
RMS Annual Session combined with the Fedorov Session 2012
Mineralogy of volcanic ash metasomatites as an indicator of island paleoarc structure type

RMS-DPI code:  2012-1-99-0
Scientific session:  M2. Mineralogical and petrological markers of the mineral/rock genesis. Minerals, ores and rocks as fingerprints
Author listing:  Yurkova R.M., Voronin B.I.
Principal author:  Yurkova Raisa M.
Language:  Russian
Abstract - Summary 
(short description):
For a vertical row of formation of forearc paleozone are typical turbidite-hemipelagic flyschoid complexes with metasomatic horizons volcaninic ash that formed subsynchronousily with volcanism. The main rock-forming mineral metasomatites is the most expressive indicator of geodynamic types paleoarc. So with calc-alkaline volcanic series pricontinental arc associated with the formation of calcium heulandite, with a bimodal spilite-keratophyre series of primitive arc - albite, with highly aluminous volcanism ensimatic arc developed - high-alumina zeolites: laumontite, and analcime.

paleoarc, volcaninic ash metasomatites, indicators, zeolites, P-T conditions.
Date of presentation:  08/10/2012
Presentation Place:  Mining University, foyer of the Assembly Hall
RMS-DPI code:  2012-1-99-0
Proceeedings volume 
in the RMS catalogue:
Mineralogy in whole space of the word.
File of proceedings 
 202 K
Status:  printed
Accepted:  28/08/2012
Published on-line:  26/10/2012
Permanent address of publication:
Contact author(s):  Yurkova, Raisa M.

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