Zobrazeno 1 - 10
of 58
pro vyhledávání: '"H. G. Stosch"'
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::561abef38875def01d4d53f491b5b489
https://doi.org/10.1016/s0016-7037(99)00178-7
https://doi.org/10.1016/s0016-7037(99)00178-7
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::08c6bc562400f425a50b02c2d99284f5
https://doi.org/10.1016/s0009-2541(97)00019-3
https://doi.org/10.1016/s0009-2541(97)00019-3
Publikováno v:
Lithos. 36:227-242
Rare lower crustal xenoliths found in Cenozoic alkali basalts from the Tariat region in central Mongolia and the Dariganga Plateau in south-eastern Mongolia are the only direct samples of lower crustal material known so far from central and eastern A
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::95d2c581ea07f03421a56b6d9be11f4c
https://doi.org/10.1016/0024-4937(95)00019-4
https://doi.org/10.1016/0024-4937(95)00019-4
Publikováno v:
Journal of Petrology. 34:1141-1175
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0db6b77644571478168b2d2a0298b8f2
https://doi.org/10.1093/petrology/34.6.1141
https://doi.org/10.1093/petrology/34.6.1141
Publikováno v:
Contributions to Mineralogy and Petrology. 110:321-328
The concentrations of titanium and rare earth elements (REE) in olivines, orthopyroxenes, clinopyroxenes and spinels from four anhydrous, spinel-bearing peridotite xenoliths have been determined. The distribution of titanium (used as an analogue for
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d7ee31a2a0eb725e8529f7c8add98dc7
https://doi.org/10.1007/bf00310747
https://doi.org/10.1007/bf00310747
Publikováno v:
Terra Nova. 4:53-62
The crust ≈ 10–20 km under the Eifel is composed of amphibolite-facies metasediments and meta-igneous rocks of tonalitic to granodioritic composition; mafic granulites occupy the base of the crust down to a Moho depth between about 29 and 34 km.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4a9d0131230d7ecd33490a2e4529b382
https://doi.org/10.1111/j.1365-3121.1992.tb00450.x
https://doi.org/10.1111/j.1365-3121.1992.tb00450.x
Publikováno v:
Contributions to Mineralogy and Petrology. 111:235-247
Anhydrous and amphibole-bearing peridotite xenoliths occur in roughly equal quantitites in the Bartoy volcanic field about 100 km south of the southern tip of Lake Baikal in Siberia (Russia). Whole-rock samples and pure mineral separates from nine xe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f595b5bd03a71c47177d29a44b784b41
https://doi.org/10.1007/bf00348954
https://doi.org/10.1007/bf00348954
Publikováno v:
Tectonophysics. 195:271-289
Crustal xenoliths in three Cenozoic volcanic fields of West Germany, the Northern Hessian Depression (NHD), the Eifel and the Urach/Hegau, include medium to high-grade meta sedimentary and felsic to mafic meta-igneous rocks. Also present in all three
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4c3cdd21edaf047a2203fcba0866498c
https://doi.org/10.1016/0040-1951(91)90215-e
https://doi.org/10.1016/0040-1951(91)90215-e
Publikováno v:
Contributions to Mineralogy and Petrology. 107:112-123
The central gneiss complex of the Munchberg Massif consists of the Liegendserie at the base and the Hangendserie at the top. Metagabbros are found in the Liegendserie; eclogites occur in the Hangendserie. New isotope data revive the discussion whethe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e2ec80ad5f97672ddac1d7d774d3cc59
https://doi.org/10.1007/bf00311189
https://doi.org/10.1007/bf00311189
Autor:
H.-G. Stosch, G. W. Lugmair
Publikováno v:
Earth and Planetary Science Letters. 99:230-249
In the Munchberg Massif in the Variscan foldbelt of southern Germany two varieties of eclogite are known which are intercalated with amphibolite-facies meta-igneous and meta-sedimentary rocks: a dark kyanite-free and a lighter colored kyanite-bearing
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c024f270e486ec0f03e7d7755da2dda5
https://doi.org/10.1016/0012-821x(90)90113-c
https://doi.org/10.1016/0012-821x(90)90113-c