£49.00

Geologische Kontrolle der Karuba-Masisi-Mineralisierung; Nord-Kivu: Geologische Kontrolle der Stano-Wolfram-Mineralisierung im Karuba-Sektor, Masisi; Nord-Kivu (östlich von DRCongo)

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Description

Die Feldstudie, die unter kartographischen, strukturellen und metallogenen Gesichtspunkten durchgeführt wurde, erlaubte festzustellen, dass der Sektor von Muvunyi Karuba (Bisunzu) im Großen und Ganzen von mehreren Netzen von Brüchen und Adern (Pegmatiten und Quarz) durchzogen ist. Die Quarzgänge durchschneiden auch die Mineralfoliation mit der Besonderheit, dass sie kataklastisch sind. Was die Brüche betrifft, so haben sie eine Vorzugsrichtung von N76°E. In Anbetracht der verschiedenen Brüche, die während der Deformationsphase, d.h. nach der Kristallisation des Magmas, auftraten, und dass durch einige dieser Brüche die hydrothermalen Lösungen kristallisierten, schließen wir, dass : das erste Netzwerk von Quarzadern resultiert aus der Kristallisation der hydrothermalen Lösungen, die hoch differenziert und reich an Siliziumdioxid sind und deren Fluidzirkulation bevorzugt durch N150°E/49°NW orientierte Brüche erfolgte, während für das zweite Netzwerk von Quarzadern die Kristallisation der Fluide bevorzugt in N10°E bis N50°E orientierten Ebenen erfolgte.

Product Specifications

Format
paperback
Domain
Amazon UK
Release Date
31 January 2021
Listed Since
01 February 2021

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