The Cretaceous Alkaline Dyke Swarm in the Central Segment of the Asunción Rift, Eastern Paraguay: Its Regional Distribution, Mechanism of Emplacement, and Tectonic Significance
Figure 5
Stereographic projection of the site mean paleomagnetic results for the alkaline dykes that occur in the central segment of the Asunción Rift. Note that the majority of the dykes acquired their remanence during a reversed polarity. Data source: [36].
