Petrologic and geophysical study of the source of long wavelength crustal magnetic anomalies.

Research output: Contribution to journalArticle

Abstract

The magnetic mineralogy and magnetic signature of banded iron formations, diagenetic (unmetamorphosed) and low grade banded iron formations, high-grade mineralogy, and phase equilibria of magnetite inorogenic magmas are discussed. -from STAR, 22(11), 1984

Original languageEnglish (US)
Journal[No source information available]
StatePublished - Jan 1 1983
Externally publishedYes

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banded iron formation
magnetic anomaly
mineralogy
wavelength
phase equilibrium
magnetite

ASJC Scopus subject areas

  • Environmental Science(all)
  • Earth and Planetary Sciences(all)

Cite this

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title = "Petrologic and geophysical study of the source of long wavelength crustal magnetic anomalies.",
abstract = "The magnetic mineralogy and magnetic signature of banded iron formations, diagenetic (unmetamorphosed) and low grade banded iron formations, high-grade mineralogy, and phase equilibria of magnetite inorogenic magmas are discussed. -from STAR, 22(11), 1984",
author = "B. Marsch and Schlinger, {Charles M}",
year = "1983",
month = "1",
day = "1",
language = "English (US)",
journal = "[No source information available]",

}

TY - JOUR

T1 - Petrologic and geophysical study of the source of long wavelength crustal magnetic anomalies.

AU - Marsch, B.

AU - Schlinger, Charles M

PY - 1983/1/1

Y1 - 1983/1/1

N2 - The magnetic mineralogy and magnetic signature of banded iron formations, diagenetic (unmetamorphosed) and low grade banded iron formations, high-grade mineralogy, and phase equilibria of magnetite inorogenic magmas are discussed. -from STAR, 22(11), 1984

AB - The magnetic mineralogy and magnetic signature of banded iron formations, diagenetic (unmetamorphosed) and low grade banded iron formations, high-grade mineralogy, and phase equilibria of magnetite inorogenic magmas are discussed. -from STAR, 22(11), 1984

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