Compositional and volume changes accompanying progressive serpentinization  of dunites from the Webster-Addie ultramafic body, North Carolina

K.C. Condie; J.A. Madison

Compositional and volume changes accompanying progressive serpentinization of dunites from the Webster-Addie ultramafic body, North Carolina

K.C. Condie^*, J.A. Madison

^*Corresponding author for this work

Research output: Contribution to journal › Article › peer-review

12 Citations (Scopus)

Abstract

Chemical and modal analyses of 22 partially serpentinized dunites from the Webster-Addie ultramafic body in North Carolina suggests losses of Mg and Fe, additions of Si and Na, and an increase in volume during progressive serpentinization of the dunites.

Original language	English
Pages (from-to)	1173-1179
Number of pages	7
Journal	American Mineralogist
Volume	54
Issue number	7-8
Publication status	Published - Jul 1969
Externally published	Yes

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title = "Compositional and volume changes accompanying progressive serpentinization of dunites from the Webster-Addie ultramafic body, North Carolina",

abstract = "Chemical and modal analyses of 22 partially serpentinized dunites from the Webster-Addie ultramafic body in North Carolina suggests losses of Mg and Fe, additions of Si and Na, and an increase in volume during progressive serpentinization of the dunites.",

author = "K.C. Condie and J.A. Madison",

year = "1969",

month = jul,

language = "English",

volume = "54",

pages = "1173--1179",

journal = "American Mineralogist",

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T1 - Compositional and volume changes accompanying progressive serpentinization of dunites from the Webster-Addie ultramafic body, North Carolina

AU - Condie, K.C.

AU - Madison, J.A.

PY - 1969/7

Y1 - 1969/7

N2 - Chemical and modal analyses of 22 partially serpentinized dunites from the Webster-Addie ultramafic body in North Carolina suggests losses of Mg and Fe, additions of Si and Na, and an increase in volume during progressive serpentinization of the dunites.

AB - Chemical and modal analyses of 22 partially serpentinized dunites from the Webster-Addie ultramafic body in North Carolina suggests losses of Mg and Fe, additions of Si and Na, and an increase in volume during progressive serpentinization of the dunites.

UR - https://www.scopus.com/pages/publications/0014539952

M3 - Article

AN - SCOPUS:0014539952

SN - 0003-004X

VL - 54

SP - 1173

EP - 1179

JO - American Mineralogist

JF - American Mineralogist

IS - 7-8

ER -

Compositional and volume changes accompanying progressive serpentinization of dunites from the Webster-Addie ultramafic body, North Carolina

Abstract

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