DISCRIMINATION BETWEEN LATE-OROGENIC, POSTOROGENIC, AND ANOROGENIC GRANITES BY MAJOR-ELEMENT COMPOSITIONS

被引:26
作者
AGRAWAL, S
机构
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D O I
10.1086/629774
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Multivariate discriminant analysis of four varieties of granites, classified a priori exclusively on field observations, provide assignment rules that, using major element compositions alone, successfully distinguish late-orogenic (LO) from post-orogenic (PO) granites related to orogeny as well as the anorogenic granites in the anorthosite/rapakivi complexes (AR) and the alkaline ring complexes (RC). Choice of major elements as good group predictors is based on a stepwise selection method with reduction of Wilk's Lambda as the selection criterion. In two-group (P and Q) discriminant analysis of the orogenic versus anorogenic, LO versus PO, and AR versus RC pairs of groups, the former in each pair has been considered as group (P). A sample is assigned to (P) when its discriminant rule, R, obtained from R = (D-i - C-i)\/\(M(i) - C-i), is a positive quantity; otherwise it is assigned to group (Q). Here D-i denotes the discriminant score of the sample, M(i) is the mean score of group (P), C-i is the cut-off value, and i = 1, 2, and 3 for the orogenic versus anorogenic, LO versus PO, and AR versus RC pairs of groups, respectively. For the orogenic versus anorogenic group, D-1 = (0.929241 Fe2O3 - 2.570311 MgO + 1.246346 Na2O + 1.266569 K2O - 11.75422), M(1) = -0.4898, and C-1 = 0.2915. For LO versus PO granites, D-2 = \-0.889609 Al2O3 + 0.777671 Fe2O3 + 2.03159 Na2O + 1.787924 K2O - 5.102003), M(2) = -1.2974, and C-2 = -0.2317, and for AR versus RC granites, D-3 (-2.820296 MgO + 1.980987 Na2O - 6.561133), M(3) = -1.1354 and C-3 = -0.0516. An unbiased estimate of misclassification obtained with the ''Jackknife'' technique permits objective classification of ''unknown'' samples, which preferably should be biotite granites with simple mineralogy.
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页码:529 / 537
页数:9
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共 30 条
[1]   MEASURES OF LOCATION OF COMPOSITIONAL DATA SETS [J].
AITCHISON, J .
MATHEMATICAL GEOLOGY, 1989, 21 (07) :787-790
[2]  
AITCHISON J, 1986, STATISTICAL ANAL COM
[3]   PETROGENETIC INTERPRETATION OF GRANITOID ROCK SERIES USING MULTICATIONIC PARAMETERS [J].
BATCHELOR, RA ;
BOWDEN, P .
CHEMICAL GEOLOGY, 1985, 48 (1-4) :43-55
[4]   THE GEOCHEMICAL CHARACTERISTICS OF GRANITOIDS IN CONTRASTING ARCS AND COMMENTS ON MAGMA SOURCES [J].
BROWN, GC ;
THORPE, RS ;
WEBB, PC .
JOURNAL OF THE GEOLOGICAL SOCIETY, 1984, 141 (MAY) :413-426
[5]   H-TYPE (HYBRID) GRANITOIDS - A PROPOSED REVISION OF THE GRANITE-TYPE CLASSIFICATION AND NOMENCLATURE [J].
CASTRO, A ;
MORENOVENTAS, I ;
DELAROSA, JD .
EARTH-SCIENCE REVIEWS, 1991, 31 (3-4) :237-253
[6]  
Chappell B.W., 1974, PAC GEOL, V8, P173
[7]   ON CORRELATION BETWEEN VARIABLES OF CONSTANT SUM [J].
CHAYES, F .
JOURNAL OF GEOPHYSICAL RESEARCH, 1960, 65 (12) :4185-4193
[8]  
CHAYES F, 1987, USE ABUSE STAT METHO, P47
[9]   NATURE AND ORIGIN OF A-TYPE GRANITES WITH PARTICULAR REFERENCE TO SOUTHEASTERN AUSTRALIA [J].
COLLINS, WJ ;
BEAMS, SD ;
WHITE, AJR ;
CHAPPELL, BW .
CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 1982, 80 (02) :189-200
[10]  
DAVIS JC, 1986, STATISTICS DATA ANAL