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Open AccessArticle


** NEW CONCEPTUAL MODEL FOR THE MAGMA-HYDROTHERMAL-TECTONIC SYSTEM OF KRAFLA, NE ICELAND 
------------------------------------------------------------

byKntur rnason (https://sciprofiles.com/profile/872382) mailto:please_loginhttps://orcid.org/0000-0001-8773-6464 

SOR, Iceland GeoSurvey, 108 Reykjavk, Iceland
_Geosciences_ 2020, _10_(1), 34; https://doi.org/10.3390/geosciences10010034
Received: 11 December 2019 / Revised: 8 January 2020 / Accepted: 16 January 2020 / Published: 19 January 2020
(This article belongs to the Special Issue Exploring and Modeling the Magma-Hydrothermal Regime ( /journalhttps://www.mdpi.com/geosciences/special_issues/magma_regime) )

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<span itemprop="publisher" content="Multidisciplinary Digital Publishing Institute"></span><span itemprop="url" content="https://www.mdpi.com/2076-3263/10/1/34"></span>
<div class="article-icons"><span class="label openaccess">Open Access</span><span class="label articletype">Article</span></div>
<h1 class="title hypothesis_container" itemprop="name">
New Conceptual Model for the Magma-Hydrothermal-Tectonic System of Krafla, NE Iceland </h1>
<div class="art-authors hypothesis_container">

by
<span class="inlineblock"><span style="white-space: nowrap"><img src="/profiles/masked-unknown-user.png" style="width: auto; height: 16px; margin-right: 3px; margin-top: -3px;"><a href="https://sciprofiles.com/profile/872382" target="_blank" rel="noopener noreferrer">Kntur rnason</a></span><sup></sup><span style="display: inline; margin-left: 5px;"></span><a class="toEncode emailCaptcha" data-author-id="2458646" href="mailto:please_login"><sup><i class="fa fa-envelope-o"></i></sup></a><a href="https://orcid.org/0000-0001-8773-6464" target="_blank" rel="noopener noreferrer"><img src="https://www.mdpi.com/img/design/orcid.png?1b5ed457ed71c59e" title="OrcID" style="position: relative; width: 13px; margin-left: 3px; max-width: 13px !important; height: auto; top: -5px;"></a></span> 
</div>
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<span style="display:block; height:6px;"></span>
<div></div>
<div style="margin: 5px 0 15px 0;" class="hypothesis_container">
<div class="art-affiliations">
<div class="affiliation">
<div class="affiliation-name ">SOR, Iceland GeoSurvey, 108 Reykjavk, Iceland</div>
</div>
</div>
</div>
<div class="bib-identity" style="margin-bottom: 10px;">
<em>Geosciences</em> <b>2020</b>, <em>10</em>(1), 34; <a href="https://doi.org/10.3390/geosciences10010034">https://doi.org/10.3390/geosciences10010034</a>
</div>
<div class="pubhistory" style="font-weight: bold; padding-bottom: 10px;">
Received: 11 December 2019 / Revised: 8 January 2020 / Accepted: 16 January 2020 / Published: 19 January 2020
</div>
<div class="belongsTo" style="margin-bottom: 10px;">
(This article belongs to the Special Issue <a href="        
    /journalhttps://www.mdpi.com/geosciences/special_issues/magma_regime
">Exploring and Modeling the Magma-Hydrothermal Regime</a>)
</div>
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<a href="https://www.mdpi.com/geosciences/geosciences-10-00034/article_deploy/html/images/geosciences-10-00034-g001.png" title="
                        <strong>Figure 1</strong><br/>
                                                    <p>A simplified tectonic map of Iceland showing the location of Krafla (black square). Red broken lines represent spreading zones. WVZ is the Western Volcanic Zone, EVZ is the Eastern Volcanic Zone, NVZ is the Northern Volcanic Zone. SISZ is the South Iceland Seismic/Transform Zone and TFZ is the Tjrnes Fracture/Transform Zone. Thin black broken lines show central volcanoes and yellow coloured areas fissure swarms.</p>
                                                ">
</a>
<a href="https://www.mdpi.com/geosciences/geosciences-10-00034/article_deploy/html/images/geosciences-10-00034-g002.png" title="
                        <strong>Figure 2</strong><br/>
                                                    <p>An overview of the Krafla area and the central part of the fissure swarm. The figure shows the visible 110 ka caldera (black), faults and fissures close to Krafla (blue), craters and eruptive fissures (orange) and geothermal manifestations (red). The figure also shows the subsidiary geothermal area in Nmafjall, south of Krafla. Coordinates are UTM, WGS84, zone 28 in km.</p>
                                                ">
</a>
<a href="https://www.mdpi.com/geosciences/geosciences-10-00034/article_deploy/html/images/geosciences-10-00034-g003.png" title="
                        <strong>Figure 3</strong><br/>
                                                    <p>A simplified geological map of Krafla. The map also shows inferred structural features discussed in this paper. Note the abundant explosion craters in the western slopes and south of Mt. Krafla. In the upper right inlet, black dots are volcanos and green strips represent fissure swarms. Coordinates are UTM WGS84 in km. (Modified from [<xref ref-type=&quot;bibr&quot; rid=&quot;B9-geosciences-10-00034&quot;>9</xref>]).</p>
                                                ">
</a>
<a href="https://www.mdpi.com/geosciences/geosciences-10-00034/article_deploy/html/images/geosciences-10-00034-g004.png" title="
                        <strong>Figure 4</strong><br/>
                                                    <p>Different parts of the fissure swarm active at different times. Blue lines are faults and fissures, yellow lines show the eastern- and westernmost faults and fissures activated in the Krafla Fires and NWSE fault south of Mnt. Krafla that moved in the Krafla Fires. The purple line marks the Hveragil gulley. Orange lines mark eruptive craters and fissures. Coordinates are UTM, WGS84, zone 28 in km.</p>
                                                ">
</a>
<a href="https://www.mdpi.com/geosciences/geosciences-10-00034/article_deploy/html/images/geosciences-10-00034-g005.png" title="
                        <strong>Figure 5</strong><br/>
                                                    <p>Different crustal spreading directions south and north of the Krafla caldera leading to an opening component in the eastern part. The inlet bottom right shows how spreading by, d, leads to opening component, c, in the east. Blue lines represent faults and fissures and purple lines eruptive fissures and craters. Coordinates are UTM WGS84 zone 28 in km.</p>
                                                ">
</a>
<a href="https://www.mdpi.com/geosciences/geosciences-10-00034/article_deploy/html/images/geosciences-10-00034-g006.png" title="
                        <strong>Figure 6</strong><br/>
                                                    <p>The location of S-wave shadows observed during the Krafla Fires (green). The red star shows approximate centre of uplift and subsidence [<xref ref-type=&quot;bibr&quot; rid=&quot;B18-geosciences-10-00034&quot;>18</xref>]. Blue lines are faults and fissures and purple lines are craters and eruptive fissures. Coordinates are UTM, WGS84, zone 28 in km.</p>
                                                ">
</a>
<a href="https://www.mdpi.com/geosciences/geosciences-10-00034/article_deploy/html/images/geosciences-10-00034-g007.png" title="
                        <strong>Figure 7</strong><br/>
                                                    <p>A de-trended residual Bouguer gravity map (mGals) of Krafla volcano. The visible 110 ka caldera rim is shown with heavy black hatched lines. An inferred buried inner caldera rim is shown with lighter black hatched lines, an inferred lower density transverse structure is shown with grey lines and a clear density boundary to the north is shown as grey broken line. The location of the lithological section in <xref ref-type=&quot;fig&quot; rid=&quot;geosciences-10-00034-f008&quot;>Figure 8</xref> is shown by straight black line (black stars are wells on the section). Blue and green lines show faults and fissures, and craters and eruptive fissures and explosion craters are shown with yellow lines. Coordinates are UTM, WGS84, zone 28 in km.</p>
                                                ">
</a>
<a href="https://www.mdpi.com/geosciences/geosciences-10-00034/article_deploy/html/images/geosciences-10-00034-g008.png" title="
                        <strong>Figure 8</strong><br/>
                                                    <p>A lithological cross-section based on drilled wells on a NS trending profile in Krafla [<xref ref-type=&quot;bibr&quot; rid=&quot;B11-geosciences-10-00034&quot;>11</xref>]. The location of the profile is shown in <xref ref-type=&quot;fig&quot; rid=&quot;geosciences-10-00034-f007&quot;>Figure 7</xref>.</p>
                                                ">
</a>
<a href="https://www.mdpi.com/geosciences/geosciences-10-00034/article_deploy/html/images/geosciences-10-00034-g009.png" title="
                        <strong>Figure 9</strong><br/>
                                                    <p>Resistivity at 200 m a.sl. (about 300 m depth) based on 1D inversion of TEM soundings. Areas where higher resistivity is observed below low resistivity are shown as red gridded (black dots are TEM soundings (reproduced from [<xref ref-type=&quot;bibr&quot; rid=&quot;B30-geosciences-10-00034&quot;>30</xref>])). The thick black hachured lines show the 110 ka caldera. Thinner black hachured lines show buried inner caldera and grey lines mark a buried transverse structure inferred from gravity. Coordinates are UTM WGS84 zone 28 in km.</p>
                                                ">
</a>
<a href="https://www.mdpi.com/geosciences/geosciences-10-00034/article_deploy/html/images/geosciences-10-00034-g010.png" title="
                        <strong>Figure 10</strong><br/>
                                                    <p>A resistivity model for Krafla from 3D inversion of MT data. Left: resistivity map at 1250 m bl. sl. The two calderas are shown as black hatched lines, purple lines mark the S-wave shadows, grey dots are earthquake epicentres and blue lines are faults and fissures. The location of the well IDDP-1 is shown as a black star. Right: 3D view from the west. The white surface shows the upper boundary of the western S-wave shadow at 3 km depth (reproduced from [<xref ref-type=&quot;bibr&quot; rid=&quot;B31-geosciences-10-00034&quot;>31</xref>]). Coordinates are UTM WGS84 zone 28 in km.</p>
                                                ">
</a>
<a href="https://www.mdpi.com/geosciences/geosciences-10-00034/article_deploy/html/images/geosciences-10-00034-g011.png" title="
                        <strong>Figure 11</strong><br/>
                                                    <p>Earthquakes located in Krafla from November 2015 to November 2016. The map also shows the location of reinjection wells (K-26 and IDDP-1) and the transverse gravity low (grey lines) (modified from [<xref ref-type=&quot;bibr&quot; rid=&quot;B32-geosciences-10-00034&quot;>32</xref>]).</p>
                                                ">
</a>
<a href="https://www.mdpi.com/geosciences/geosciences-10-00034/article_deploy/html/images/geosciences-10-00034-g012.png" title="
                        <strong>Figure 12</strong><br/>
                                                    <p>P-wave velocity (km/s) at 0.5 km bl.sl. (left) and at 2 km bl.sl. (right) according to recent seismic tomography (reproduced from [<xref ref-type=&quot;bibr&quot; rid=&quot;B34-geosciences-10-00034&quot;>34</xref>]). Black hatched lines show the two calderas, grey lines mark the low-density transverse structure, blue lines show faults and fissures and the purple lines mark the S-wave shadows. Coordinates are UTM WGS84 zone 28 in km.</p>
                                                ">
</a>
<a href="https://www.mdpi.com/geosciences/geosciences-10-00034/article_deploy/html/images/geosciences-10-00034-g013.png" title="
                        <strong>Figure 13</strong><br/>
                                                    <p>Drilled wells in Krafla (red dot on the little inlet map to the right) and the three main production fields (right) with different thermal character. The fields are: Vtsmr and Leribotnar (blue frame), southern and western slopes of Mt. Krafla (red frame) and Hvthlar (purple frame). To the left are shown characteristic temperature profiles in wells in each production area and a well drilled in the fissure swarm west of Hvthlar. For well KS-01, east of Hvthlar, see text.</p>
                                                ">
</a>
<a href="https://www.mdpi.com/geosciences/geosciences-10-00034/article_deploy/html/images/geosciences-10-00034-g014.png" title="
                        <strong>Figure 14</strong><br/>
                                                    <p>Left; The locations and tracks of wells in Krafla (green lines) and the location of the cross-section to the right (black line). Right; A resistivity cross-section with alteration mineralogy and formation temperature in wells.</p>
                                                ">
</a>
<a href="https://www.mdpi.com/geosciences/geosciences-10-00034/article_deploy/html/images/geosciences-10-00034-g015.png" title="
                        <strong>Figure 15</strong><br/>
                                                    <p>Two-dimensional modelling of thermo-hydraulic states of geothermal systems developed after the emplacement of an 800 m wide dike intrusion extending up to 2 km below surface into rocks with a temperature gradient of 100 C/km (the scale of the horizontal and vertical axis is in km). To the left, is the system 5 ka after emplacement into rocks with the permeability 1 mD. The temperature (C) is shown by black contours and the pressure (bars) by yellow contours. Phase conditions (water/steam) are shown by colours (light blue is pure water and dark red is almost pure steam, (actual scale 10 times the logarithm of water saturation). Mass flow (kg/m<sup>2</sup>/year) is shown by arrows (scale at the bottom of the figures), blue for water phase and red for steam phase. The graph shows temperature profiles from hypothetical wells at different distances from the centre of the intrusion (related by colour) in the upper-right corners. The thick yellow line marks region of superheated steam and the green line a region with supercritical conditions. To the right, is shown a thermo-hydraulic situation 3 ka after an intrusion is placed in a host rock of permeability 1 mD, underlying a 1 km thick pile (thick grey line) of much higher permeability (50 mD in this case).</p>
                                                ">
</a>
<a href="https://www.mdpi.com/geosciences/geosciences-10-00034/article_deploy/html/images/geosciences-10-00034-g016.png" title="
                        <strong>Figure 16</strong><br/>
                                                    <p>A zoom-in on residual Bouguer gravity in and around the inner caldera. Blue lines show faults and fissures, green lines mark the boundaries of the part of the fissure swarm that was active in the Krafla Fires and an ESE-WNW fault in the southern slopes of Mt. Krafla that moved in the Krafla Fires. Yellow arcs and lines show explosion craters and eruptive fissures. Note, the abundant explosion craters west and south of Mt. Krafla. Grey lines mark the transverse structure and purple lines mark the extent of high-temperature alteration at 200 m a.sl. (from <xref ref-type=&quot;fig&quot; rid=&quot;geosciences-10-00034-f009&quot;>Figure 9</xref>). Coordinates are UTM WGS84 zone 28 in km.</p>
                                                ">
</a>
<a href="https://www.mdpi.com/geosciences/geosciences-10-00034/article_deploy/html/images/geosciences-10-00034-g017.png" title="
                        <strong>Figure 17</strong><br/>
                                                    <p>The beginning of a flow test of IDDP-1 (photo G. . Frileifsson).</p>
                                                ">
</a>
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