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A Geochemical Classification for Feldspathic Igneous Rocks
AGeochemical Classification for
Feldspathic Igneous Rocks
B. RONALD FROST* AND CAROL D. FROST
DEPARTMENT OF GEOLOGY AND GEOPHYSICS, UNIVERSITY OF WYOMING, LARAMIE, WY 82072, USA
RECEIVED MAY 13, 2008; ACCEPTED OCTOBER 3, 2008
ADVANCE ACCESS PUBLICATION NOVEMBER 20, 2008
In this paper we classify the range of feldspathic igneous rocks
using five geochemical variables: the FeO/(FeOtMgO) ratio or
Fe-index, the modified alkali^lime index, the aluminum-saturation
index, the alkalinity index, and the feldspathoid silica-saturation
index.The Fe-index distinguishes between melts that have undergone
extensive iron enrichment during differentiation from those that have
not.The transition from tholeiite to ferrobasalt allows us to extend
this boundary to silica values as low as 48 wt %.We introduce the
feldspathoid silica-saturation index, which, coupled with the alkali-
nity index, allows us to extend the geochemical classification to
alkaline rocks. We show that most alkaline rocks are ferroan and
that this probably reflects extensive fractional crystallization of
olivine and pyroxene with minimal participation of Fe^Ti oxides.
The expanded classification allows us to illustrate the geochemical
and petrogenetic relationship of the plutonic rocks from ferroan gran-
ites to nepheline syenites that commonly occur in intracratonic envir-
onments. It also allows us to distinguish four families of feldspathic
rocks: (1) magnesian rocks, which are exemplified by Caledonian
and Cordilleran batholiths and are characterized by differentiation
under oxidizing and relatively hydrous conditions; (2) ferroan rocks,
which include fayalite granites, alkali granites, and nepheline sye-
nites and are characterized by differentiation under reducing and
relatively dry conditions; (3) leucogranites, which commonly form
by crustal melting; (4) potassic and ultrapotassic rocks, which origi-
nate from mantle that has been enriched in K2O.
KEY WORDS: granite; rhyolite; geochemistry; classification;
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