A likely reason for the appearance of the Daly Gap in magmatic series of large igneous provinces: Geological and petrological evidence
Abstract
The problem of the Daly Gap is considered for the example of bimodal basalt–trachyte series and their intrusive analogs (layered syenite–gabbro intrusions). It is shown that the gap is not controlled by the processes of crystallization differentiation or liquid immiscibility in intermediate chambers of igneous systems (intrusive chambers) and has a primary nature. We interpret its origin as from the existence of two independent types of melts...
Paper Details
Title
A likely reason for the appearance of the Daly Gap in magmatic series of large igneous provinces: Geological and petrological evidence
Published Date
Feb 1, 2017
Journal
Volume
472
Issue
2
Pages
231 - 236
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