Genesis of Ultrapotassic Rocks

Part of the Springer Geology book series (SPRINGERGEOL)


Different hypotheses, invoked during the first half of the last century, involved, (1) assimilation between different magma types and rocks (Daly 1910, 1933; Shand 1931), (2) Subtraction of Eclogite from a Picrite or Peridotite Magma (Holmes 1932; O’Hara and Yoder 1967), (3) gaseous transport (Kennedy 1955), (4) zone refining process (Harris 1957), and (5) partial melting of phlogopite–richterite-bearing peridotitic mantle (Gupta and Yagi 1980).


Source Rock Partial Melting Oceanic Crust Mantle Source Crustal Contamination 
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© Springer India 2015

Authors and Affiliations

  1. 1.Mineralogy and PetrologyUniversity of AllahabadAllahabadIndia

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