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Publikováno v:
Tectonophysics. 198:112-115
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1a649b955d173029fbde9a504cb77b08
https://doi.org/10.1016/0040-1951(91)90136-g
https://doi.org/10.1016/0040-1951(91)90136-g
Autor:
B. Velde, Stephen Hillier
Publikováno v:
Clay Minerals. 26:149-168
The chemical composition of about 500 diagenetic chlorites, determined by electron microprobe, has been studied in six different sedimentary sequences spanning conditions from early diagenesis to low-grade metamorphism, in the temperature range 40–
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::75f491a268c9e2304909f7d919a36ddf
https://doi.org/10.1180/claymin.1991.026.2.01
https://doi.org/10.1180/claymin.1991.026.2.01
Autor:
Bruce B. Velde, Alain Meunier
Of course such a book as we propose here is not the product of just two people working together, although the experience has been a great pleasure for us. We would like to thank our many collaborators and students who have encouraged our effort by th
Publikováno v:
56th EAEG Meeting.
In order to provide a better understanding of sedimentary basin development, it is very important to describe correctly the evolution of the various physical, mechanical and hydraulic properties of clayey rocks as a function of burial depth. As a con
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::112a6ecf18491475fd13082d2b7c72f6
https://doi.org/10.3997/2214-4609.201410218
https://doi.org/10.3997/2214-4609.201410218
Autor:
B. Velde, O.J. Tveit
Publikováno v:
SPE Health, Safety and Environment in Oil and Gas Exploration and Production Conference.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5f895ec5a5498dfa1632d0399717cca2
https://doi.org/10.2118/23246-ms
https://doi.org/10.2118/23246-ms
Publikováno v:
Clay Minerals; Jun2008, Vol. 43 Issue 2, p185-193, 9p
Autor:
B. Velde
Publikováno v:
Journal of Geophysical Research. 99:15649
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c3ac8a40990296a0f4a9ff03183c631f
https://doi.org/10.1029/94jb00663
https://doi.org/10.1029/94jb00663
Publikováno v:
Physics and Chemistry of Minerals. 13:91-95
Raman microprobe (RMP) spectra were produced for each of the olivine and spinel structured phases of Mg2GeO4 and (Mg, Fe)2SiO4. The assembled data show that bands due to the tetrahedra in silicate and germanate olivines shift in a way that indicates
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d0c013b3134700fe5d3f216fa445972d
https://doi.org/10.1007/bf00311898
https://doi.org/10.1007/bf00311898