ScholarLens Back to search
2016•Abstracts with programs - Geological Society of AmericaRequires access

COEVAL ULTRAMAFIC, CARBONATITIC, AND FELSIC ROCKS ARE ASSOCIATED WITH MAGNETITE DEPOSITS IN THE HUDSON HIGHLANDS OF NEW YORK: A CASE OF MULTIPLE ANATECTIC MELTS

Robert F. Martin, Marian Lupulescu

Open publisher page 0 citations

Abstract

This record does not include an abstract. Use the full-text link above if available.

About this research paper

What this paper is about

An abstract is not available in the OpenAlex record for this paper.

Why it matters

A significance statement is not available in the OpenAlex record.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Key concepts: Ultramafic rock, Felsic, Magnetite, Geology, Geochemistry, Petrology, Mafic, Paleontology

Related papers

Related paper 1Related paper 2
Back to paper searchBrowse research topicsOriginal source
COEVAL ULTRAMAFIC, CARBONATITIC, AND FELSIC ROCKS ARE ASSOCIATED WITH MAGNETITE DEPOSITS IN THE HUDSON HIGHLANDS OF NEW YORK: A CASE OF MULTIPLE ANATECTIC MELTS — Research Paper | ScholarLens