Evolution of the assemblage magnesite and quartz by metasomatic reactions within metadolomites during retrograde metamorphism in the southern Damara Orogen : Namibia / D. Puhan; S. Fillie; N. Henkel.

By:

Puhan, D

Contributor(s):

Fillie, S.Henkel, N

Material type: Text

TextLanguage: English Series: Communications of the Geological Survey of Namibia special commemorative issue. Vol.12 S. ; FilliePublication details: Windhoek : Nam Print, 2002Description: P.4 : sketches, illustrations, graph; 30 cmSubject(s):

DDC classification:

PER 553 Communications of the Geological Survey of Namibia

Summary: A long lasting fluid infiltration event influenced mineral reactions during retrograde metamorphism in parts of the southern margin zone of the Damara Orogen.

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Books	Namibia Scientific Society Library		Not for loan

References on page 102.

A long lasting fluid infiltration event influenced mineral reactions during retrograde metamorphism in parts of the southern margin zone of the Damara Orogen.

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