Oxygen isotope ratios and rare earth element (REE) concentrations provide independent tests of competing models of injection v. anatexis for the origin of migmatites from amphibolite and granulite facies metasedimentary rocks of the Adirondack Mountains
Late Proterozoic mafic magmatism was widespread in the Adirondack region of New York State, and was ...
The metamorphic record provides a key element for understanding the development of mountain belts an...
The Byram Intrusive Suite granite gneisses of the New Jersey Highlands are believed to be similar in...
ABSTRACT Oxygen isotope ratios and rare earth element (REE) concentrations provide independent tests...
Oxygen isotope ratios and rare earth element (REE) concentrations provide independent tests of compe...
The Adirondack Mountains, New York, expose a diverse group of Proterozoic igneous rocks that were me...
Elemental and carbon isotope analysis was performed on the distinctive marginal garnet sillimanite g...
The Adirondack Mountains in upstate New York contain exposures of complex partially melted rocks, in...
The Mount Eve granite suite is a postorogenic, A-type granitoid suite that consists of several small...
The metamorphosed monzonitic to granitic gneiss suite of the Adirondack highlands is spatially and ...
The Adirondack Highlands contain dominantly meta-igneous rocks including the anorthosite-granite as...
Quantitative estimates of metamorphic fluid speciation, stable isotopic analyses, and studies of flu...
the highlands lying south-east of the Carthage-Colton mylonite zone (CCMZ, Fig. 1) and the lowlands ...
The 1010 Ma Canada Hill Granite represents a small post-orogenic granitoid body that can be found in...
PhDGeochemistryUniversity of Michigan, Horace H. Rackham School of Graduate Studieshttp://deepblue.l...
Late Proterozoic mafic magmatism was widespread in the Adirondack region of New York State, and was ...
The metamorphic record provides a key element for understanding the development of mountain belts an...
The Byram Intrusive Suite granite gneisses of the New Jersey Highlands are believed to be similar in...
ABSTRACT Oxygen isotope ratios and rare earth element (REE) concentrations provide independent tests...
Oxygen isotope ratios and rare earth element (REE) concentrations provide independent tests of compe...
The Adirondack Mountains, New York, expose a diverse group of Proterozoic igneous rocks that were me...
Elemental and carbon isotope analysis was performed on the distinctive marginal garnet sillimanite g...
The Adirondack Mountains in upstate New York contain exposures of complex partially melted rocks, in...
The Mount Eve granite suite is a postorogenic, A-type granitoid suite that consists of several small...
The metamorphosed monzonitic to granitic gneiss suite of the Adirondack highlands is spatially and ...
The Adirondack Highlands contain dominantly meta-igneous rocks including the anorthosite-granite as...
Quantitative estimates of metamorphic fluid speciation, stable isotopic analyses, and studies of flu...
the highlands lying south-east of the Carthage-Colton mylonite zone (CCMZ, Fig. 1) and the lowlands ...
The 1010 Ma Canada Hill Granite represents a small post-orogenic granitoid body that can be found in...
PhDGeochemistryUniversity of Michigan, Horace H. Rackham School of Graduate Studieshttp://deepblue.l...
Late Proterozoic mafic magmatism was widespread in the Adirondack region of New York State, and was ...
The metamorphic record provides a key element for understanding the development of mountain belts an...
The Byram Intrusive Suite granite gneisses of the New Jersey Highlands are believed to be similar in...