Zobrazeno 1 - 10
of 87
pro vyhledávání: '"Eero Hanski"'
Autor:
Yao Bi, Huan Chen, Eero Hanski, Takeshi Kuritani, Hong-Xiang Wu, Feng-Qi Zhang, Jia Liu, Xiao-Yan Gu, Qun-Ke Xia
Publikováno v:
Scientific Reports, Vol 14, Iss 1, Pp 1-12 (2024)
Abstract Recent research on the water content of large igneous provinces (LIPs) has revealed that water has a significant impact on the formation of LIPs. However, most studies focus on the water content of mafic–ultramafic rocks, while relatively
Externí odkaz:
https://doaj.org/article/58115f26b4114255937e286267102122
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 24, Iss 7, Pp n/a-n/a (2023)
Abstract Water is critical in the evolution of the mantle due to its strong influence on the physicochemical properties of mantle rocks. Mid‐ocean ridge basalts (MORBs) are commonly used to study the compositional characteristics of the convecting
Externí odkaz:
https://doaj.org/article/15d7e5e2fbbc41649aee5b37327ee746
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 92, Iss 2, Pp 131-150 (2020)
The Kivilompolo molybdenite occurrence is located in the northern part of the Peräpohja belt, within the lithodemic Ylitornio nappe complex. It is hosted within a deformed porphyritic granite belonging to the pre-orogenic 1.99 Ga Kierovaara suite. T
Externí odkaz:
https://doaj.org/article/1a481704ccc340af9b22956e7619c8af
Autor:
Kimmo Kärenlampi, Asko Kontinen, Eero Hanski, Hannu Huhma, Yann Lahaye, Joachim Krause, Thomas Heinig
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 92, Iss 1, Pp 39-71 (2020)
The Otanmäki area in central Finland hosts two occurrences of Nb-Zr-REE minerali-zation, Katajakangas and Kontioaho, within a suite of ca. 2.04–2.06 Ga (A1-type) gneissic granites, syenite and monzonite-monzodiorite. They exhibit trace element cha
Externí odkaz:
https://doaj.org/article/0e6c3230fd474900af18a964b7fe412c
Autor:
Eero Hanski, Hannu Huhma, Yann Lahaye, Juha Pekka Lunkka, Erik Nilsson, Timo Mäki, Hugh O´Brien, Kari Strand
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 91, Iss 2, Pp 143-178 (2019)
Over the past tens of years, glacial sandstone erratics variably enriched in Zn, Pb and Cu have been collected from the coast south of Raahe, but their source has remained ambiguous. In these non-metamorphosed and non-deformed boulders, detrital grai
Externí odkaz:
https://doaj.org/article/aaf9a608138e43fb879f6bad99565537
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 91, Iss 1, Pp 35-73 (2019)
The 2.05 Ga Otanmäki suite represents a globally rare occurrence of Paleoproterozoic non-orogenic A1-type magmatism. It consists of a broad variety of A-type felsic and intermediate igneous rocks including monzodiorites, monzonites, syenites and per
Externí odkaz:
https://doaj.org/article/9e3aa73561bf4a49ad7c2fe6e0a75373
Publikováno v:
Nature Communications, Vol 8, Iss 1, Pp 1-8 (2017)
The genesis of large igneous provinces (LIPs) remains controversial. Here, the authors examine the water contents of picrites from the Emeishan LIP and find that despite high water contents, the elevated temperature and trace elements suggest a mantl
Externí odkaz:
https://doaj.org/article/7055bf3a2e9e491d94ff03d88de09ac3
Autor:
Валерий Федорович Смолькин, Ееро Хански, Ханну Хухма, Жорж Александрович Федотов, Valery Smolkin, Eero Hanski, Hannu Huhma, Zhorzh Fedotov
Publikováno v:
Transactions of the Karelian Research Centre of the Russian Academy of Sciences, Vol 0, Iss 7, Pp 74-84 (2015)
The Nyasyukka dike complex forms a NW-trending dike swarm in the Archean bedrock of the Murmansk Province adjacent to the Pechenga Complex. The dikes are mostly composed of two rock types, kaersutite-bearing peridotites and olivine gabbros. Also a ro
Externí odkaz:
https://doaj.org/article/7cb9b66c33cd48d484984666342c45be
Autor:
Fang-Fang Guo, Wolfgang D. Maier, Jussi S. Heinonen, Eero Hanski, Jouni Vuollo, Sarah-Jane Barnes, Yann Lahaye, Hannu Huhma, Shenghong Yang
Publikováno v:
Lithos. :107206
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2875582c88076c4d0745e68c0e46e289
https://doi.org/10.1016/j.lithos.2023.107206
https://doi.org/10.1016/j.lithos.2023.107206
Autor:
Matthew Goode, Jukka-Pekka Ranta, Timo Mäki, Ballinteer Park, Ballinteer, Dublin , D Hk , Ireland, Holly J. Stein, Eero Hanski, Näsilinnankatu D , Tampere, Finland, Atte Taivalkoski
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 92, Iss 2, Pp 131-150 (2020)
The Kivilompolo molybdenite occurrence is located in the northern part of the Peräpoh jabelt, within the lithodemic Ylitornio nappe complex. It is hosted within a deformed porphyritic granite belonging to the pre-orogenic 1.99 Ga Kierovaara suite. T
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0f7289d850e228ff5e3246191869116f
https://www.geologinenseura.fi/sites/geologinenseura.fi/files/bulletin_vol92_2_131-150_ranta-etal.pdf
https://www.geologinenseura.fi/sites/geologinenseura.fi/files/bulletin_vol92_2_131-150_ranta-etal.pdf