Multi-tiered, disrupted crust of a sheet lava flow from the Diveghat Formation of Deccan Traps: Implications on emplacement mechanisms
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DOI: 10.1007/s12040-020-01418-9
Abstract: The crust is a vesicular layer that caps the compact core of sheet lava flows. We describe for the first time, a crust composed of multiple layers (each distinguished by a chilled glassy rind) from… read more here.
Keywords: diveghat formation; sheet; lava flow; sheet lava ... See more keywords