Zobrazeno 1 - 10
of 101
pro vyhledávání: '"R. A. WIEBE"'
Autor:
Qiqi Yang, Ben Wang, Phillipe Lemey, Lu Dong, Tong Mu, R. Alex Wiebe, Fengyi Guo, Nídia Sequeira Trovão, Sang Woo Park, Nicola Lewis, Joseph L.-H. Tsui, Sumali Bajaj, Yachang Cheng, Luojun Yang, Yuki Haba, Bingying Li, Guogang Zhang, Oliver G. Pybus, Huaiyu Tian, Bryan Grenfell
Publikováno v:
Nature Communications, Vol 15, Iss 1, Pp 1-13 (2024)
Abstract Highly pathogenic avian influenza virus (HPAIV) A H5, particularly clade 2.3.4.4, has caused worldwide outbreaks in domestic poultry, occasional spillover to humans, and increasing deaths of diverse species of wild birds since 2014. Wild bir
Externí odkaz:
https://doaj.org/article/6a127744872b4dc9a3789c73d17d0bdb
Autor:
Qiqi Yang, Ben Wang, Phillipe Lemey, Lu Dong, Tong Mu, R. Alex Wiebe, Fengyi Guo, Nídia Sequeira Trovão, Sang Woo Park, Nicola Lewis, Joseph Tsui, Sumali Bajaj, Yachang Cheng, Luojun Yang, Yuki Haba, Bingying Li, Guogang Zhang, Oliver G. Pybus, Huaiyu Tian, Bryan Grenfell
Highly pathogenic avian influenza virus (HPAIV) A H5 clade 2.3.4.4 has caused worldwide outbreaks in domestic poultry, occasional spillover to humans, and increasing deaths of diverse species of wild birds since 2014. Wild bird migration is currently
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5deda59075e3043a2ff9227ab60b08e4
https://doi.org/10.1101/2023.05.22.541648
https://doi.org/10.1101/2023.05.22.541648
Publikováno v:
Contributions to Mineralogy and Petrology. 165:1275-1294
The catastrophic eruption of large-volume, crystal-rich silicic magmas is often proposed to be a consequence of reheating, melting and overturn of partially molten, buoyant silicic material following repeated injection of dense, hot mafic magma. To t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dc6b3af8c48f3807001f954db261fb35
https://doi.org/10.1007/s00410-013-0858-5
https://doi.org/10.1007/s00410-013-0858-5
Publikováno v:
Contributions to Mineralogy and Petrology. 154:439-453
The Vinalhaven intrusive complex provides field and petrographic evidence for multiple replenishments of mafic and silicic magmas, mingling and limited mixing, and rejuvenation of granite. Quartz in granitic rocks preserves a record of those processe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d63e29b32b6309ffb065768467501d69
https://doi.org/10.1007/s00410-007-0202-z
https://doi.org/10.1007/s00410-007-0202-z
Publikováno v:
Lithos. 93:234-247
The Gouldsboro Granite forms part of the Coastal Maine Magmatic Province, a region characterized by granitic plutons that are intimately linked temporally and petrogenetically with abundant co-existing mafic magmas. The pluton is complex and preserve
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::52e40baabdc64dcfe15b3e05bfe5c553
https://doi.org/10.1016/j.lithos.2006.03.066
https://doi.org/10.1016/j.lithos.2006.03.066
Publikováno v:
Contributions to Mineralogy and Petrology. 153:121-138
Schlieren that form above the solidus are potentially diagnostic of the rheology of crystallizing granitic magmas and could provide insights into mag- ma chamber structure. Here we focus on steep schlie- ren associated with comagmatic enclaves in the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d364d0ecdd0f4c7f69cc4fcd300036da
https://doi.org/10.1007/s00410-006-0142-z
https://doi.org/10.1007/s00410-006-0142-z
Publikováno v:
Journal of Petrology. 45:2133-2153
The Vinalhaven intrusive complex consists mainly of coarse-grained granite, inward-dipping gabbro–diorite sheets, and a fine-grained granite core. Small bodies of porphyry occur throughout the coarsegrained granite. The largest porphyry body (rough
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9b3f3f6a101d4c66fc2c18f9d1194f83
https://doi.org/10.1093/petrology/egh050
https://doi.org/10.1093/petrology/egh050
Autor:
J. Warner Cribb, Daniel S. Lazzareschi, R. A. Wiebe, Nicole L. Cates, Brian E. Harper, G. Christopher Koteas, Calvin F. Miller
Publikováno v:
Earth and Environmental Science Transactions of the Royal Society of Edinburgh. 95:277-295
The mid-Miocene Aztec Wash pluton is divisible into a relatively homogeneous portion entirely comprising granites (the G zone, or GZ), and an extremely heterogeneous zone (HZ) that includes the products of the mingling, mixing and fractional crystall
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::231f0fe4fcb5dd50796a29174f4c0570
https://doi.org/10.1017/s0263593300001073
https://doi.org/10.1017/s0263593300001073
Publikováno v:
Geological Society of America Bulletin. 114:909-920
Located in the northern Sierra Nevada, the Middle Jurassic Pyramid Peak granite and associated dioritic rocks display superbly exposed interlayered sheets of mafic, felsic, and hybrid rocks. The mafic-hybrid layers show a consistent asymmetry (sharpl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9125837868f2763bea9d1fa430cc094b
https://doi.org/10.1130/0016-7606(2002)114<0909:miisha>2.0.co
https://doi.org/10.1130/0016-7606(2002)114<0909:miisha>2.0.co
Publikováno v:
Contributions to Mineralogy and Petrology. 142:323-335
The Pleasant Bay layered gabbro-diorite complex (420 Ma) formed via repeated injections of mafic magma into a felsic magma chamber. It is dominated by repeating sequences (macrorhythmic units) with chilled gabbroic bases which may grade upward into m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::13cab2456d52d446ffe60da00a4537bd
https://doi.org/10.1007/s004100100292
https://doi.org/10.1007/s004100100292