Browsing ELibrary by Author "Foley S.F."
- DSpace Home
- →
- Геология России
- →
- ELibrary
- →
- Browsing ELibrary by Author
JavaScript is disabled for your browser. Some features of this site may not work without it.
Browsing ELibrary by Author "Foley S.F."
Now showing items 1-13 of 13
-
Bottazzi P.; Tiepolo M.; Vannucci R.; Zanetti A.; Brumm R.; Foley S.F.; Oberti R. (1999)New experimental amphibole/melt partition coefficients from a variety of geologically relevant amphibole (pargasite, kaersutite, and K-richterite) and melt compositions obtained under conditions of interest to upper-mantle ...
-
Tappe S.; Foley S.F.; Jenner G.A.; Kjarsgaard B.A. (2005)We introduce a modification to the current IUGS classification system for igneous rocks to include ultramafic lamprophyres, which are currently entirely omitted. This is done by including a new step in the sequential system, ...
-
Stalder R.; Foley S.F.; Drey G.P.; Horn I. (1998)In order to constrain the role of fluid phases during metasomatic processes in the upper mantle, trace element partition coefficients for Ba, Sr, Pb, Nb, Ta, Zr, Hf, Ti, La, Ce, Sm, Tb, and Yb between aqueous fluids and ...
-
Stalder R.; Foley S.F.; Brey G.P.; Horn I. (1998)In order to constrain the role of fluid phases during metasomatic processes in the upper mantle, trace element partition coefficients for Ba, Sr, Pb, Nb, Ta, Zr, Hf, Ti, La, Ce, Sm, Tb, and Yb between aqueous fluids and ...
-
Barth M.G.; Foley S.F.; Horn I. (2002)The partitioning of an extensive suite of trace elements between garnet, clinopyroxene, and hydrous tonalitic melts has been studied experimentally at 1.8 GPa and 1000–1040°C. The knowledge of trace element partitioning ...
-
Melzer S.; Foley S.F. (2000)Liquidus phase relations in the system diopside–kalsilite–forsterite–quartz with 3 wt% F were examined at 1 bar and the locations of important invariant points were determined at 18 kbar. At all pressures within this range ...
-
Melzer S.; Foley S.F. (2000)Liquidus phase relations in the system diopside-kalsilite-forsterite-quartz with 3 wt% F were examined at 1 bar and the locations of important invariant points were determined at 18 kbar. At all pressures within this range ...
-
Foley S.F.; Barth M.G.; Jenner G.A. (2000)Fractionation of some or all of the high field strength elements (HFSE) Nb, Ta, Zr, Hf, and Ti relative to other trace elements occurs in igneous rocks from convergent margins and in the average continental crust, and is ...
-
Schafer F.N.; Foley S.F. (2002)The effect of crystal anisotropy on wetting angles of equilibrium silicate melts on crystal faces of spinel, diopside, enstatite and olivine has been determined experimentally by the sessile melt drop technique. The ...
-
Foley S.F. (1985)Olivine leucitites from the Gaussberg volcano, Antarctica are primitive members of the lamproite group of ultrapotassic rocks. They are glass rich, have an Mg number of around 70, and carry spinel lherzolite xenoliths. ...
-
Foley S.F.; Taylor W.R.; Green D.H. (1986)The effects of H2O, CO2, CH4 and HF on partial melting of a model phlogopite harzburgite mantle are considered with regard to the production of ultrapotassic magmas. Fluorine has a polymerising effect in H2O-poor conditions, ...
-
Foley S.F.; Venturelli G.; Green D.H.; Toscani L. (1987)A definition for ultrapotassic rocks is introduced using the chemical screens K2O > 3 wt.%, MgO > 3 wt.% and K2O/Na2O > 2 for whole-rock analyses. On this basis a data base of more than 800 analyses was retrieved by a ...
-
Glaser S.M.; Foley S.F.; Günther D. (1999)Peridotite xenoliths from the Bereya alkali picrite tuff in the Vitim volcanic province of Transbaikalia consist of garnet lherzolite, garnet-spinel lherzolite and spinel lherzolite varieties. The volcanism is related to ...
Now showing items 1-13 of 13
Search DSpace
Browse
-
All of DSpace
-
This Collection