Published 1987 | Version v1
Miscellaneous Metadata-only

Isotope studies of the serpentinization of ultramafic rocks

Creators

  • 1. Akademie der Wissenschaften der DDR, Leipzig. Zentralinstitut fuer Isotopen- und Strahlenforschung
  • 2. AN SSSR, Moscow. Geologicheskij Inst.

Description

δD and δ18O variations as well as hydrogen contents of serpentinites, chrysotile asbestos, garnet pyroxenites and garnetite were investigated. The garnet serpentinites (mean δD = -1050/00) and also the garnet pyroxenites and garnetite (mean δD = -420/00) have rather uniform δD values. The δD and δ18O values of garnet serpentinites and crysotile asbestos give hints that these rocks were formed by interaction with magmatic water but at different temperatures. The formation conditions of the garnet serpentinites from the Saxonian Granulite Massif and from the Saxonian Ore Mts. have obviously been analogous. (author)

Additional details

Publishing Information

Imprint Title
Proceedings of the Fourth Working Meeting Isotopes in Nature
Imprint Pagination
688 p.
Journal Page Range
p. 143-149.

Conference

Title
4. working meeting isotopes in nature.
Dates
22-26 Sep 1986.
Place
Leipzig (German Democratic Republic).

INIS

Country of Publication
German Democratic Republic
Country of Input or Organization
German Democratic Republic
INIS RN
19091469
Subject category
S37: INORGANIC, ORGANIC, PHYSICAL AND ANALYTICAL CHEMISTRY;
Resource subtype / Literary indicator
Conference, Non-conventional Literature
Descriptors DEI
DEUTERIUM; GEOCHEMISTRY; ISOTOPE RATIO; MINERALS; OXYGEN 18; ROCKS
Descriptors DEC
EVEN-EVEN NUCLEI; HYDROGEN ISOTOPES; ISOTOPES; LIGHT NUCLEI; NUCLEI; ODD-ODD NUCLEI; OXYGEN ISOTOPES; STABLE ISOTOPES