Vol. 294, Issue 9, 1994November 01, 1994 EDT
Are Stable Isotopic Trends in Amphibolite to Granulite Facies Transitions Metamorphic or Diagenetic?; an Answer for the Arendal Area (Bamble Sector, Southeastern Norway) From mid-Proterozoic Carbon-Bearing Rocks
Are Stable Isotopic Trends in Amphibolite to Granulite Facies Transitions Metamorphic or Diagenetic?; an Answer for the Arendal Area (Bamble Sector, Southeastern Norway) From mid-Proterozoic Carbon-Bearing Rocks
Broekmans, M. A. T. M., Nijland, T. G., & Ben H. Jansen, J. (1994). Are stable isotopic trends in amphibolite to granulite facies transitions metamorphic or diagenetic?; an answer for the Arendal area (Bamble Sector, southeastern Norway) from mid-Proterozoic carbon-bearing rocks. American Journal of Science, 294(9), 1135–1165. https://doi.org/10.2475/ajs.294.9.1135
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