1,720,964 research outputs found
Resource Map Series - Specific Identified Resources at the uppermost 50 m of the pretertiary basement
No full textMap of Specific Identified Resources for 50m upper part of the pre-Tertiary basement (map scale 1:500 000). See the Summary Report "Geothermal Models at Supra-Regional Scale", Goetzl Gregor & Zekiri Fatime (2012), for specific details on the methodologies and approaches applied.TRANSENERGY - Central Europe 2007 - 201
Resource Map Series - Specific Identified Resources from surface until 5000 m.b.s.
No full textMap of Specific Identified Resources from surface until 5000 m.b.s (map scale 1:500 000). See the Summary Report "Geothermal Models at Supra-Regional Scale", Goetzl Gregor & Zekiri Fatime (2012), for specific details on the methodologies and approaches applied.TRANSENERGY - Central Europe 2007 - 201
Temperature Map Series - Temperature at depth of 1000 m below surface
No full textDistribution of subsurface temperatures at depth levels of 1000m below surface (map scale: 1:500 000). See the Summary Report "Geothermal Models at Supra-Regional Scale", Goetzl Gregor & Zekiri Fatime (2012), for specific details on the methodologies and approaches applied.TRANSENERGY - Central Europe 2007 - 201
Resource Map Series - Specific Heat in Place from surface until 7000 m.b.s
No full textMap of Specific Heat in Place from surface until 7000 m.b.s (map scale 1:500 000). See the Summary Report "Geothermal Models at Supra-Regional Scale", Goetzl Gregor & Zekiri Fatime (2012), for specific details on the methodologies and approaches applied.TRANSENERGY - Central Europe 2007 - 201
Resource Map Series - Specific Identified Resources for neogene sediments
No full textMap of Specific Identified Resources for Neogene sediments (map scale 1:500 000). See the Summary Report "Geothermal Models at Supra-Regional Scale", Goetzl Gregor & Zekiri Fatime (2012), for specific details on the methodologies and approaches applied.TRANSENERGY - Central Europe 2007 - 201
Temperature Map Series - Temperature at depth of 2500 m below surface
No full textDistribution of subsurface temperatures at depth level of 2500 m below surface (map scale 1:500 000). See the Summary Report "Geothermal Models at Supra-Regional Scale", Goetzl Gregor & Zekiri Fatime (2012), for specific details on the methodologies and approaches applied.TRANSENERGY - Central Europe 2007 - 201
Depth Contour Map Series - Depths of 50 degC isothermal surface
No full textDepth contour map of the 50°C isotherm (map scale 1:500 000). See the Summary Report "Geothermal Models at Supra-Regional Scale", Goetzl Gregor & Zekiri Fatime (2012), for specific details on the methodologies and approaches applied.TRANSENERGY - Central Europe 2007 - 201
Depth Contour Map Series - Depths of 150 degC isothermal surface
No full textDepth contour map of the 150°C isotherm (map scale 1:500 000). See the Summary Report "Geothermal Models at Supra-Regional Scale", Goetzl Gregor & Zekiri Fatime (2012), for specific details on the methodologies and approaches applied.TRANSENERGY - Central Europe 2007 - 201
Going Beyond Counting First Authors in Author Co-citation Analysis
Get PDFThe present study examines one of the fundamental aspects of author co-citation analysis (ACA) - the way co-citation
counts are defined. Co-citation counting provides the data on which all subsequent statistical analyses and mappings
are based, and we compare ACA results based on two different types of co-citation counting - the traditional type that
only counts the first one among a cited work's authors on the one hand and a non-traditional type that takes into
account the first 5 authors of a cited work on the other hand. Results indicate that the picture produced through this non-traditional author co-citation counting contains more coherent author groups and is therefore considerably clearer. However, this picture represents fewer specialties in the research field being studied than that produced through the traditional first-author co-citation counting when the same number of top-ranked authors is selected and analyzed. Reasons for these effects are discussed
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