Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Lanbin Shi"'
Publikováno v:
Science China Earth Sciences. 53:1295-1306
The trachyandesite lavas from Heikongshan volcano of the Tengchong volcanic cluster, Yunnan Province contain relatively abundant mafic and ultramafic small xenoliths comprising mainly gabbro, pyroxenite and rare lherzolites, all less than 2.5 cm in s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::766d96a4c52eb35cd85c766a928a6e92
https://doi.org/10.1007/s11430-010-4044-6
https://doi.org/10.1007/s11430-010-4044-6
Publikováno v:
The Journal of Geology. 112:593-605
Cenozoic basalts from both sides of the Daxin’anling‐Taihang gravity lineament that separates the Sino‐Korean craton (SKC) into western and eastern parts have been studied. In the western SKC, magmas evolved from xenolith‐bearing alkali basal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::511335a4bb8105b810a3eba528fa0f38
https://doi.org/10.1086/422668
https://doi.org/10.1086/422668
Publikováno v:
Lithos. 47:181-193
The Qilin geotherm established by Xu et al. [Xu, X.S., O'Reilly, S.Y., Zhou, X.M. and Griffin, W.L., 1996. A xenolith-derived geotherm and the crust-mantle boundary at Qilin, southeastern China. Lithos, 38: 41–62.] using the Ellis and Green [Ellis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e99bd082ac4e6e9b093659726380b42f
https://doi.org/10.1016/s0024-4937(99)00014-6
https://doi.org/10.1016/s0024-4937(99)00014-6
Publikováno v:
Science in China Series D: Earth Sciences. 41:171-178
The paleogeotherm derived from spinel and garnet lherzolites xenoliths for the upper mantle beneath Zhejiang Province, China is higher than the oceanic geotherm but is similar to the geotherm for the upper mantle beneath eastern China constructed by
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2edebbd6027d66b502089ffd9fae494f
https://doi.org/10.1007/bf02932437
https://doi.org/10.1007/bf02932437
Publikováno v:
Acta Seismologica Sinica. 10:365-373
The Koktokay-Ertai fault zone was developed on the basis of a former ductile shear zone (mylonite zone). The mylonites were formed in the brittle-ductile transition zone at 10–15 km depth within the crust. The rocks had experienced multi period def
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d9f1bc3e88e46dda2389e74a58cb783e
https://doi.org/10.1007/s11589-997-0075-2
https://doi.org/10.1007/s11589-997-0075-2
Autor:
J. C. C. Mercier, Chuanyong Lin, Martin Menzies, Yi-Gang Xu, John V. Ross, Ben Harte, Lanbin Shi
Publikováno v:
Contributions to Mineralogy and Petrology. 125:406-420
Ultramafic xenoliths in Cenozoic alkali basalts from Yitong, northeast China comprise three types in terms of their modal mineralogy: lherzolite, pyroxenite and wehrlite. The wehrlite suite always contains interstitial pale/brown glass which occupies
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b9d647b9b5482c4226c5038319410840
https://doi.org/10.1007/s004100050231
https://doi.org/10.1007/s004100050231
Publikováno v:
Journal of Geology. Sep2004, Vol. 112 Issue 5, p593-605. 13p.