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Calculation and application of clinopyroxene-garnet-plagioclase-quartz geobarometers

Moecher, D. P., Essene, E. J., Anovitz, L. M.·1988·Contributions to Mineralogy and Petrology
DOI 10.1007/bf00399441
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  • Pressure estimates based on metamorphic mineral assemblages across most of the major shear zones do not show measurable vertical displacements within the uncertainty of the geobarometers.

    “However, pressure estimates based on metamorphic mineral assemblages across most of the major shear zones do not show measurable vertical displacements within the uncertainty ( + 1 kbar or about _+ 3 kin) of the geobarometers”

    From U-Pb geochronology of the Grenville Orogen of Ontario and New York: constraints on ancient crustal tectonics (1993) · cites this paper as Moecher et al. 1988

  • The boundary between the Central Metasedimentary and Central Gneiss Belt shows metamorphic pressures apparently increasing over a short distance from about 6 kbar in the Bancroft domain to about 8 kbar in the eastern Central Gneiss Belt.

    “except for the boundary between the Central Metasedimentary and Central Gneiss Belt (Fig. 2) where metamorphic pressures apparently increase over a short distance from about 6 kbar in the Bancroft domain to about 8 kbar in the eastern Central Gneiss Belt.”

    From U-Pb geochronology of the Grenville Orogen of Ontario and New York: constraints on ancient crustal tectonics (1993) · cites this paper as Moecher et al. 1988

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Authors
Moecher, D. P., Essene, E. J., & Anovitz, L. M.
Venue
Contributions to Mineralogy and Petrology
Publisher
Springer Science and Business Media LLC
Published
1988-09
Volume
100
Issue
1
Pages
92-106
ISSN
  • 0010-7999
  • 1432-0967
DOI
10.1007/bf00399441
Cited by
215
References
0
Language
en
Licence
www.springer.com/tdm (tdm)

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