Closure temperature (Tc) of a geochronological system may be defined as its temperature at the time corresponding to its apparent age. For thermally activated diffusion in which R is the gas constant, E the activation energy, z the time constant with which the diffusion coefficient D diminishes, a
β¦ LIBER β¦
Closure temperature in cooling geochronological and petrological systems
β Scribed by Martin H. Dodson
- Publisher
- Springer
- Year
- 1973
- Tongue
- English
- Weight
- 887 KB
- Volume
- 40
- Category
- Article
- ISSN
- 0010-7999
No coin nor oath required. For personal study only.
π SIMILAR VOLUMES
Closure temperature in cooling geochrono
β
Martin H. Dodson
π
Article
π
1973
π
Springer
π
English
β 887 KB
Alpine metamorphic evolution and cooling
β
BalΓ‘zs Koroknai; PΓ©ter HorvΓ‘th; Kadosa Balogh; IstvΓ‘n Dunkl
π
Article
π
2001
π
Springer
π
English
β 581 KB
Erratum to: Alpine metamorphic evolution
β
BalΓ‘zs Koroknai; PΓ©ter HorvΓ‘th; Kadosa Balogh; IstvΓ‘n Dunkl
π
Article
π
2001
π
Springer
π
English
β 10 KB
Opening and resetting temperatures in he
β
Emmanuel GardΓ©s; Jean-Marc Montel
π
Article
π
2009
π
Springer
π
English
β 481 KB
Eo-alpine metamorphism in the uppermost
β
Eberhard Seidel; Martin Okrusch; Hans Kreuzer; Helmut Raschka; Wilhelm Harre
π
Article
π
1981
π
Springer
π
English
β 1012 KB
The uppermost unit of the Cretan nappe system consists of ophiolites on the top, and an ophiolitic m61ange at the base. Among the various constituents of the m61ange, there are slices of low-P/high-T metamorphics. They form a variegated series consisting of tholeiitic ortho-amphibolites, para-amphi
Discovery of khondalite series from the
β
Jianxin Zhang; Zeming Zhang; Zhiqin Xu; Jingsui Yang; Junwen Cui
π
Article
π
2000
π
Science in China Press (SCP)
π
English
β 545 KB