Structural and Subsurface Relationships between the Fort Rixon Greenstone Belt and the Nalatale Granite Pluton, Zimbabwe, as derived from Gravity and Aeromagnetic Data.

R.T. Ranganai

doi:10.3997/2214-4609-pdb.143.4.2

Structural and Subsurface Relationships between the Fort Rixon Greenstone Belt and the Nalatale Granite Pluton, Zimbabwe, as derived from Gravity and Aeromagnetic Data.
By R.T. Ranganai
Publisher: European Association of Geoscientists & Engineers
Source: Conference Proceedings, 7th SAGA Biennial Technical Meeting and Exhibition, Oct 2001, cp-143-00017
DOI: https://doi.org/10.3997/2214-4609-pdb.143.4.2

Abstract

The late-Archaean Fort Rixon greenstone belt is one of the smallest greenstone belts of the<br>Zimbabwe craton, with a maximum length of ~20 km and a width of ~10 km. According to Harrison (1969),<br>it can be imagined that successive periods of intrusion and granitisation have encroached upon the belt,<br>causing a progressive decrease in its size.

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2001-10-09

2025-01-15

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Structural and Subsurface Relationships between the Fort Rixon Greenstone Belt and the Nalatale Granite Pluton, Zimbabwe, as derived from Gravity and Aeromagnetic Data.

Abstract

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