14°56′34″S26°3′21″E / 14.94278°S 26.05583°E / -14.94278; 26.05583
The Hook granite massif is a large formation in central Zambia formed around 550 million years ago during the Pan-African orogeny.
It lies in the inner part of the Lufilian arc.[1]
Today, the south-western extension of the massif lies under the Kafue National Park.[2]
^Cite error: The named reference Hanson1999 was invoked but never defined (see the help page).
^D.B. Fanshawe (December 2010). "VEGETATION DESCRIPTIONS OF THE UPPER ZAMBEZI DISTRICTS OF ZAMBIA" (PDF). Biodiversity Foundation for Africa. Retrieved 2012-06-08.
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14°56′34″S 26°3′21″E / 14.94278°S 26.05583°E / -14.94278; 26.05583 The Hookgranitemassif is a large formation in central Zambia formed around 550 million...
of felsic or intermediate rock types, such as granite, quartz monzonite, or diorite (see also granite dome). Although they may appear uniform, batholiths...
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direction of folding, between the Zambezi Belt and the Lufilian Arc. The Hookgranitemassif, in the inner arc just north of the Mwembeshi Shear Zone, is a large...
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