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Research Article|
February 01, 1991
Comment and Reply on "Nd isotopic gradients in upper crustal magma chambers: Evidence for in situ magma-wall-rock interaction"
Benjamin C. Schuraytz;
Benjamin C. Schuraytz
1
Lunar and Planetary Institute, 3303 NASA Road 1, Houston, Texas 77058
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Thomas A. Vogel;
Thomas A. Vogel
2
Department of Geological Sciences, Michigan State University, East Lansing, Michigan 48824
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Leland W. Younker;
Leland W. Younker
3
Earth Sciences Department, Lawrence Livermore National Laboratory, Livermore, California 94550
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G. Lang Farmer;
G. Lang Farmer
4
CIRES and Department of Geological Sciences, University of Colorado, Boulder, Colorado 80309
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Kathryn J. Tegtmeyer
Kathryn J. Tegtmeyer
4
CIRES and Department of Geological Sciences, University of Colorado, Boulder, Colorado 80309
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Geology (1991) 19 (2): 185–187.
Article history
first online:
02 Jun 2017
Citation
Benjamin C. Schuraytz, Thomas A. Vogel, Leland W. Younker, G. Lang Farmer, Kathryn J. Tegtmeyer; Comment and Reply on "Nd isotopic gradients in upper crustal magma chambers: Evidence for in situ magma-wall-rock interaction". Geology ; 19 (2): 185–187. doi: https://doi.org/10.1130/0091-7613(1991)019<0185:CARONI>2.3.CO;2
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Index Terms/Descriptors
- ash-flow tuff
- Cenozoic
- crust
- geochemistry
- igneous rocks
- isotopes
- magma chambers
- magmas
- metals
- metasomatism
- Miocene
- Nd-144/Nd-143
- neodymium
- Neogene
- Nevada
- Paintbrush Tuff
- pumice
- pyroclastics
- rare earths
- stable isotopes
- Tertiary
- Topopah Spring Member
- trace elements
- United States
- upper crust
- volcanic rocks
- wall-rock alteration
Latitude & Longitude