Zobrazeno 1 - 10
of 21
pro vyhledávání: '"H. A. Seck"'
Publikováno v:
Contributions to Mineralogy and Petrology. 148:511-523
Patches of glass with a second generation of small crystals of olivine, clinopyroxene, and spinel are abundant in hydrous peridotite mantle xenoliths with tabular equigranular textures from two maar-type volcanoes, Meerfelder Maar and Dreiser Weiher
Autor:
Herbert Palme, H. A. Seck, Karl-Ludwig Kratz, Gudrun Witt-Eickschen, Gerhard Schmidt, Bernhard Spettel
Publikováno v:
Chemical Geology. 196:77-105
Mantle peridotite xenoliths ranging in modal composition between fertile lherzolites and modally metasomatized harzburgites, and magmatic pyroxenite xenoliths from the West Eifel and Vogelsberg volcanic fields (Germany) have been analyzed for their w
Publikováno v:
European Journal of Mineralogy. 15:95-102
Publikováno v:
Geochimica et Cosmochimica Acta. 64:99-115
Partition coefficients of the rare earth elements (REE) and the high field strength elements (HFSE: Ti, Zr, Hf, Nb, Ta) among clinopyroxenes, garnets, and andesitic to granodioritic melts were experimentally determined at pressures ranging from 1 to
Publikováno v:
Chemical Geology. 138:257-271
The knowledge of rare-earth element (REE) and high field-strength element (HFSE) partitioning between minerals such as amphibole, pyroxenes or garnet and tonalitic liquids is essential to understand where and how tonalitic melts are generated. In thi
Publikováno v:
Contributions to Mineralogy and Petrology. 124:71-81
The extremely young (2.5 Ma) I-type Eldzhurtinskiy granite complex (Central Caucasus) is uniform with respect to modal composition, major and trace element chemistries of bulk rocks and mineral phases. In contrast, it reveals two types of alkali feld
Publikováno v:
European Journal of Mineralogy. 8:607-624
Publikováno v:
Journal of Petrology. 34:1141-1175
Publikováno v:
Journal of Petrology. 34:1-22
Autor:
H. A. Seck, G. Witt-Eickschen
Publikováno v:
Contributions to Mineralogy and Petrology. 106:431-439
Geothermometric equations for spinel peridotites by Fujii (1976), Gasparik and Newton (1984), and Chatterjee, and Terhart (1985) based on the reaction enstatite (en)+spinel (sp)→Mg−Tschermaks (mats)+forsterite (fo) were tested using a nearly isot