| 1. | The last magmatism identified is the Jersey Dyke Swarm from.
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| 2. | The Okavango Dyke Swarm overlaps with the Lebombo and Large Igneous Province.
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| 3. | Intrusion of Okavango Dyke Swarm occurred in two distinct stages.
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| 4. | Both radial and linear dyke swarm configurations exist.
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| 5. | Huge dyke swarms are formed in radial geometry.
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| 6. | Giant dyke swarms having lengths > 300 km are a common record of severely eroded LIPs.
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| 7. | The Jersey Main Dyke Swarm consists of dolerite dykes intruded into the South East Igneous complex.
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| 8. | By the time of intrusion of the Florida dyke swarm, Piedra Alta Terrane was experiencing extensional tectonics.
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| 9. | The number of Jurassic dykes accumulates, hence a giant dyke swarm can be developed in the region.
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| 10. | The "'Uruguayan dyke swarms "'consist of three groups of tectono-stratigraphic terrane.
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