Asiantuntijatarkastetut julkaisut

Permanent URI for this collectionhttp://hdl.handle.net/10138/579122

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    Influence of HfO2 control oxide ALD precursor chemistry for nitride memories
    (2011) Nikolaou, N.; Dimitrakis, P.; Normand, P.; Ioannou-Sougleridis, V.; Giannakopoulos, K.; Mergia, K.; Kukli, Kaupo; Niinistö, Jaakko; Ritala, Mikko; Leskelä, Markku; Geologian tutkimuskeskus; Geological Survey of Finland
    Tiivistelmä
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    Justus GTK Helda testi 17.9.2024
    (Wiley, 2024) Marttila, Hannu; Kløve, Bjørn; Geologian tutkimuskeskus; Geological Survey of Finland
    Tiedosto vaihdettu
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    Late Weichselian to Holocene history of the Baltic Sea as reflected in ostracod assemblages
    (Francis & Taylor, 2019) Stepanova, Anna; Obrochta, Stephen; Quintana Krupinski, Nadine B.; Hyttinen, Outi; Kotilainen, Aarno; Andrén, Thomas; Geologian tutkimuskeskus; Geological Survey of Finland
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    Environmental impact of mineralised black shales
    (Elsevier, 2019) Parviainen, Annika; Loukola-Ruskeeniemi, Kirsti; Geologian tutkimuskeskus; Geological Survey of Finland
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    Integrated Object-Based Image Analysis for semi-automated geological lineament detection in southwest England
    (Elsevier, 2019) Yeomans, Christopher M.; Middleton, Maarit; Shail, Robin K.; Grebby, Stephen; Lusty, Paul A.J.; Geologian tutkimuskeskus; Geological Survey of Finland
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    Magnetotelluric array in the central Finnish Lapland I: Extreme data characteristics
    (Elsevier, 2020) Autio, U.A.; Smirnov, M.Yu.; Geologian tutkimuskeskus; Geological Survey of Finland
    We present magnetotelluric (MT) data from the northern Fennoscandian shield, which show extreme behavior due to the complex geoelectric setting left behind by the tectonic reworking of the Archaean bedrock during the Palaeoproterozoic. The core of the MT data set from the central Finnish Lapland were acquired in 2014 in the context of the MaSca-project. Extreme data are defined by the condition where the determinant of the real and/or imaginary part of the impedance tensor becomes negative. This is related to, but is a more anomalous condition than out-of-quadrant off-diagonal impedance phases. Physically, these are associated to reversal of e.g. the electric field as compared to its direction for one-dimensional resistivity structure. So far, only few examples of extreme data have been explicitly reported in geophysical literature. Data previously classified as erroneous might belong to the class of extreme data instead and data quality analysis should take this into account. A resistivity contrast of at least ca. 1:1000 is required to observe extreme data, as indicated by synthetic modelling studies. Extreme data are challenging from a modelling point of view and thus also drive the need for new developments in forward and inverse codes for MT.
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    A geologically-based approach to map arsenic risk in crystalline aquifers: Analysis of the Tampere region, Finland
    (Elsevier BV; Zhongguo Dizhi Daxue, 2019) Pedretti, Daniele; Luoma, Samrit; Ruskeeniemi, Timo; Backman, Birgitta; 0000-0001-7677-3948; Geologian tutkimuskeskus; Geological Survey of Finland
    The study illustrates the critical role of accurate geological structural mapping to delineate crystalline aquifer zones more prone to high health risk due to elevated dissolved As in drinking wells. The analysis revisits the results from more than 1200 groundwater samples collected over ten years from domestic wells across the Tampere region (Finland).
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    Justus GTK Helda testi 3
    (Marine Geological Institute, 2016) Rahardiawan, Riza; Purwanto, Catur; 0000-0001-5109-3700; 0000-0001-5109-3701; Geologian tutkimuskeskus; Geological Survey of Finland
    Lorem ipsum dolor sit amet, consectetur adipiscing elit. Donec erat nulla, facilisis at eros et, convallis semper tellus. Curabitur viverra neque non justo porttitor maximus. Sed tempor lectus at nisl volutpat, non hendrerit metus facilisis. Etiam auctor nulla ut massa vehicula, eget rutrum sem egestas. Ut posuere vel velit a lacinia. Aliquam blandit blandit tristique. Pellentesque semper ipsum tincidunt mi vestibulum lacinia. Aliquam placerat lorem ac mi rhoncus, accumsan commodo nulla bibendum.
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    Justus GTK testi
    (Wiley, 2014) Marttila, Hannu; Kløve, Bjørn; Geologian tutkimuskeskus; Geological Survey of Finland