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Evolution of the Continental Upper Mantle : Numerical Modelling of Thermo-chemical Convection Including Partial Melting

This thesis elaborates on the evolution of the continental upper mantle based on numerical modelling results. The descriptive and explanatory basis is formed by a numerical thermo-chemical convection model. The model evolution starts in the early Archaean about 4 billion years ago. The model follows from the conservation equations, which are based on the physical laws describing the upper mantle. Several simplifications have been made as is common practice in model studies. Nowadays, modern high- and top-end computers pave the way for these increasingly realistic simulations. Qualitative scenarios can now be tested and furthermore modelling may reveal new dynamical concepts, which had not been proposed.

Ketersediaan
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Balai Besar Survei dan Pemetaan Geologi Kelautan - Jln. Dr. Djundjunan No. 236, Bandung, Jawa Barat BSL 551.24 SME e
BSL 551.24 SME e
Tersedia
Informasi Detail
Judul Seri
Geologica Ultraiectina
No. Panggil
BSL 551.24 SME e
Penerbit
Utrecht : Utrecht University.,
Deskripsi Fisik
pp. 1 - 137
Bahasa
English
ISBN/ISSN
90-5744-029-6
Klasifikasi
551.24
Tipe Isi
-
Tipe Media
-
Tipe Pembawa
-
Edisi
172
Subjek
Evolution of the continental upper mantle : numeri
Info Detail Spesifik
-
Pernyataan Tanggungjawab
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