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Molybdenum systematics of subducted crust record extensive, reactive flow from underlying slab-serpentine dehydration

Autor: Chen, S., Hin, R.C., John, T., Brooker, R., Bryan, B., Niu, Y.L, Elliott, T.

Publikováno v: Nature communications, 2019, Vol.10, pp.4773 [Peer Reviewed Journal]

Fluids liberated from subducting slabs are critical in global geochemical cycles. We investigate the behaviour of Mo during slab dehydration using two suites of exhumed fragments of subducted, oceanic lithosphere. Our samples display a positive corre

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od_______328::1c0287590ed3637f4bb94b165d37d56f
http://dro.dur.ac.uk/29345/2/29345.pdf

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Ophiolites in the Xing’an-Inner Mongolia accretionary belt of the CAOB : implications for two cycles of seafloor spreading and accretionary orogenic events

Autor: Song, S.G., Wang, M.J., Xu, X., Wang, C., Niu, Y.L., Allen, M.B., Su, L.

Publikováno v: Tectonics, 2015, Vol.34(10), pp.2221-2248 [Peer Reviewed Journal]

The Xing'an-Inner Mongolia accretionary belt in the southeastern segment of the Central Asian Orogenic Belt (CAOB) was produced by the long-lived subduction and eventual closure of the Paleo-Asian Ocean and by the convergence between the North China

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od_______328::bcc0a750561cac05ec03f75978568027
http://dro.dur.ac.uk/18114/1/18114.pdf

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Mantle sources and petrogenesis of the Cenozoic basalts in Fanshi, Shanxi province : geochemical and Sr-Nd-Pb-Hf isotopic evidence

Autor: Ye, L., Liu, J.J., Niu, Y.L., Guo, P.Y., Sun, P., Cui, H.X.

Publikováno v: 岩石学报. = Acta petrologica Sinica, 2015, Vol.31(1), pp.161-175 [Peer Reviewed Journal]

The Fanshi basalts located in the vicinity of the Da Hinggan Ling-Taihangshan gravity gradient zone, represent a major component of Cenozoic basalts of the central North China Craton. Previous studies gave the Fanshi basalts whole rock K-Ar ages of 2

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od_______328::56dd3f3d6a6e9984566bfd1335542211
http://dro.dur.ac.uk/15898/1/15898.pdf

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Trace element budgets and (re-)distribution during subduction-zone ultrahigh pressure metamorphism : evidence from Western Tianshan, China

Autor: Xiao, Y.Y., Niu, Y.L., Li, H.K., Wang, H.C., Liu, X.M., Davidson, J.P.

Publikováno v: Chemical geology, 2014, Vol.365, pp.54-68 [Peer Reviewed Journal]

We have conducted an LA-ICP-MS in situ trace element study of garnet, epidote group minerals, phengitic muscovite and paragonite in rocks of basaltic and sedimentary protolith from an ultrahigh pressure metamorphic belt along Western Tianshan, China.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od_______328::ab156257cd6c4dfeaf19a5b4b801e31f

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Akademický článek

The stable vanadium isotope composition of the mantle and mafic lavas

Autor: Prytulak, J., Nielsen, S.G., Ionov, D.A., Halliday, A.N., Harvey, J., Kelley, K.A., Niu, Y.L., Peate, D.W., Shimizu, K., Sims, K.W.W.

Publikováno v: In Earth and Planetary Science Letters 1 March 2013 365:177-189

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Zircon records of Miocene ultrapotassic rocks from southern Lhasa subterrane, Tiben Plateau

Autor: Liu, D., Zhao, Z.D., Zhu, D.C., Niu, Y.L., Liu, S.A., Wang, Q., Liu, Y.S., Hu, Z.C.

Publikováno v: 岩石学报. = Acta petrologica Sinica, 2013, Vol.29(11), pp.3703-3715 [Peer Reviewed Journal]

Zircons entrained in mantle-derived magmas offer a prime opportunity to reveal cryptic magmatic episodes in the deep crust. We have investigated zircons from mantle-derived ultrapotassic veins in the Xuena area, southern Lhasa subterrane. Zircons in

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od_______328::f67f320591a63bb4a2397586635c6602
http://dro.dur.ac.uk/15772/1/15772.pdf

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U-Th-Ra disequilibria and the extent of off-axis volcanism across the East Pacific Rise at 9°30′N, 10°30′N, and 11°20′N

Autor: Turner, S., Beier, C., Niu, Y.L., Cook, C.

Publikováno v: Geochemistry, geophysics, geosystems, 2011, Vol.12(7), pp.Q0AC12 [Peer Reviewed Journal]

There is widespread interest in the distance that mid-ocean ridge magmatism extends beyond the neovolcanic zone. Off-axis magmas also provide a means to map out variations across the melting zone. We present 238U-230Th-226Ra data for 35 well-characte

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od_______328::c91bec6f097dd032dd2fe73d24b77aa4

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Geochemistry, geochronology and petrogenesis of East Kunlun high Nb-Ta rhyolites

Autor: Ding, S., Huang, H., Niu, Y.L., Zhao, Z.D., Yu, X.H., Mo, X.X.

Publikováno v: 岩石学报. = Acta petrologica Sinica, 2011, Vol.27(12), pp.3603-3614 [Peer Reviewed Journal]

The East Kunlun high Nb-Ta rhyolite is located at the eastern end of the Kunlun orogenic belt. Zircon U-Pb analysis gives a magmatic age of about 213Ma, corresponding to the subduction/collision stage of the Kunlun Orogeny. Compared to the felsic vol

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od_______328::b29ebee312bfec48c18e707c370da756
http://dro.dur.ac.uk/15958/1/15958.pdf

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Akademický článek

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