where the range is from the state back-arc to either radiating swarms or vice versa originating from igneous centers.
https://homeworkmarkets.com/wp-content/uploads/2020/08/logo1-300x75.png 0 0 Mike https://homeworkmarkets.com/wp-content/uploads/2020/08/logo1-300x75.png Mike2023-12-01 10:59:392023-12-01 10:43:27respectively. The coeval sills found mostly in Zimbabwe and the Kaapvaal cratons have a close relationship to each other. These sills are however the feeders to the south pans berg group of lavas at presumable facts (Olsson and S""Oderlund et al. 490--500). The dated feeder dyke systems are the source of the new information thus being the source code to the cause of petronic setting re-evaluation
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