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DEPENDENCE OF REDUCED INTENSITY OF THERMOLUMINESCENCE OF ROCKS ON THEIR ABSOLUTE AGE, AS SEEN IN GRANITOIDS FROM SOVIET CENTRAL ASIA.

Author
SAMOYLOV YU A; SAMOJLOV YU A; TOLKUNOV A YE; TOLKUNOV AE
IGEM/MOSKVA
Source
DOKL. EARTH SCI. SECT.; U.S.A.; DU RUSSE: DOKL. AKAD. NAUK S.S.S.R., S.S.S.R. 1974; 214, NO 3, 666-668,1974, VOL. 214, P. 175 A 176
Document type
Miscellaneous
Language
English; Russian
Keyword (fr)
K-AR DATATION THERMOLUMINESCENCE GRANITOIDE ASIE CENTRALE URSS GEOCHIMIE ISOTOPIQUE GEOLOGIE SCIENCES DE LA TERRE URSS
Keyword (en)
K AR DATING DATING THERMOLUMINESCENCE GRANITOID CENTRAL ASIA USSR ISOTOPE GEOCHEMISTRY GEOLOGY EARTH SCIENCES
Keyword (es)
GEOQUIMICA ISOTOPICA GEOLOGIA CIENCIAS DE LA TIERRA
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences

Discipline
Earth sciences
Origin
Inist-CNRS ; BRGM
Database
PASCAL
INIST identifier
PASCALGEODEBRGM7620032161

Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS

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