Probable regional geothermal field reconnaissance in the Aegean region from modern multi-temporal night LST imagery
Identifieur interne : 000007 ( PascalFrancis/Checkpoint ); précédent : 000006; suivant : 000008Probable regional geothermal field reconnaissance in the Aegean region from modern multi-temporal night LST imagery
Auteurs : D. Zouzias [Grèce] ; George Ch. Miliaresis [Grèce] ; K. St. Seymour [Canada]Source :
- Environmental earth sciences : (Print) [ 1866-6280 ] ; 2011.
Descripteurs français
- Pascal (Inist)
- Champ géothermique, Actuel, Imagerie, Satellite, Température surface, Pixel, Modèle numérique élévation, Distribution spatiale, Arc volcanique, Enthalpie, Interprétation, Télédétection spatiale, Anomalie thermique, Volcan, Granodiorite, Pluton, Puits forage, Mer Ionienne, Crète, Ile Milos, Iles Dodécanèse, Mer Egée.
- Wicri :
- topic : Satellite, Interprétation, Mer Ionienne.
English descriptors
- KwdEn :
- Aegean Sea, Crete, Dodecanese, Ionian Sea, Milos, Pixel, Space remote sensing, boreholes, digital elevation models, enthalpy, geothermal fields, granodiorites, imagery, interpretation, modern, plutons, satellites, spatial distribution, surface temperature, thermal anomalies, volcanic arcs, volcanoes.
Abstract
The Hellenic Peninsula and the adjacent Aegean and Ionian seas are segmented into regions on the basis of Terra satellite-MODIS instrument derived land surface temperatures (LST) to test if they can be used in the field reconnaissance for potential geothermal targets, each region representing a different thermal signature. The method has been used successfully to identify hot spot and geothermal activity in the Afar Triangle and in the Red Sea. Night monthly average LST values per pixel, since 2001, are used in this work for geothermal field identification. Average LST seasonal variability is expressed by a common centroid curve of pixel cluster. Clusters were subsequently ranked in increasing LST according to their centroids. Cluster-2 represents by far the Aegean volcanic arc (AVA) which comprises the high enthalpy (320 and 350°C, respectively) geothermal fields of Milos and Nisyros. The interpretation of LST terrain segmentation into sub-clusters of Cluster-2 is consistent with thermal anomalies related to the volcano-islands of the AVA, the occurrence of thermal anomalies related to granodiorite plutons in the Cyclades and to the volcano-related anomalies of the Dodecanese Province. We conclude that the identification of such thermal anomalies obtained by a combination of remote sensing (LST), regional geology and field data (borehole, thermal spring and subsurface hydrothermal reservoir temperatures) can be a particularly useful exploration tool for localizing geothermal anomalies.
Affiliations:
Links toward previous steps (curation, corpus...)
Links to Exploration step
Pascal:11-0166701Le document en format XML
<record><TEI><teiHeader><fileDesc><titleStmt><title xml:lang="en" level="a">Probable regional geothermal field reconnaissance in the Aegean region from modern multi-temporal night LST imagery</title><author><name sortKey="Zouzias, D" sort="Zouzias, D" uniqKey="Zouzias D" first="D." last="Zouzias">D. Zouzias</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Department of Geology, University of Patras</s1><s2>26504 Rion</s2><s3>GRC</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ></inist:fA14><country>Grèce</country><wicri:noRegion>26504 Rion</wicri:noRegion></affiliation></author><author><name sortKey="Miliaresis, George Ch" sort="Miliaresis, George Ch" uniqKey="Miliaresis G" first="George Ch." last="Miliaresis">George Ch. Miliaresis</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Department of Geology, University of Patras</s1><s2>26504 Rion</s2><s3>GRC</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ></inist:fA14><country>Grèce</country><wicri:noRegion>26504 Rion</wicri:noRegion></affiliation></author><author><name sortKey="Seymour, K St" sort="Seymour, K St" uniqKey="Seymour K" first="K. St." last="Seymour">K. St. Seymour</name><affiliation wicri:level="1"><inist:fA14 i1="02"><s1>Department of Geography, Urban Planning and Environment, Concordia University</s1><s2>Montreal, QC H3G1M8</s2><s3>CAN</s3><sZ>3 aut.</sZ></inist:fA14><country>Canada</country><wicri:noRegion>Montreal, QC H3G1M8</wicri:noRegion></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">INIST</idno><idno type="inist">11-0166701</idno><date when="2011">2011</date><idno type="stanalyst">PASCAL 11-0166701 INIST</idno><idno type="RBID">Pascal:11-0166701</idno><idno type="wicri:Area/PascalFrancis/Corpus">000011</idno><idno type="wicri:Area/PascalFrancis/Curation">000029</idno><idno type="wicri:Area/PascalFrancis/Checkpoint">000007</idno><idno type="wicri:explorRef" wicri:stream="PascalFrancis" wicri:step="Checkpoint">000007</idno></publicationStmt><sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">Probable regional geothermal field reconnaissance in the Aegean region from modern multi-temporal night LST imagery</title><author><name sortKey="Zouzias, D" sort="Zouzias, D" uniqKey="Zouzias D" first="D." last="Zouzias">D. Zouzias</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Department of Geology, University of Patras</s1><s2>26504 Rion</s2><s3>GRC</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ></inist:fA14><country>Grèce</country><wicri:noRegion>26504 Rion</wicri:noRegion></affiliation></author><author><name sortKey="Miliaresis, George Ch" sort="Miliaresis, George Ch" uniqKey="Miliaresis G" first="George Ch." last="Miliaresis">George Ch. Miliaresis</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Department of Geology, University of Patras</s1><s2>26504 Rion</s2><s3>GRC</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ></inist:fA14><country>Grèce</country><wicri:noRegion>26504 Rion</wicri:noRegion></affiliation></author><author><name sortKey="Seymour, K St" sort="Seymour, K St" uniqKey="Seymour K" first="K. St." last="Seymour">K. St. Seymour</name><affiliation wicri:level="1"><inist:fA14 i1="02"><s1>Department of Geography, Urban Planning and Environment, Concordia University</s1><s2>Montreal, QC H3G1M8</s2><s3>CAN</s3><sZ>3 aut.</sZ></inist:fA14><country>Canada</country><wicri:noRegion>Montreal, QC H3G1M8</wicri:noRegion></affiliation></author></analytic><series><title level="j" type="main">Environmental earth sciences : (Print)</title><title level="j" type="abbreviated">Environ. earth sci. : (Print)</title><idno type="ISSN">1866-6280</idno><imprint><date when="2011">2011</date></imprint></series></biblStruct></sourceDesc><seriesStmt><title level="j" type="main">Environmental earth sciences : (Print)</title><title level="j" type="abbreviated">Environ. earth sci. : (Print)</title><idno type="ISSN">1866-6280</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Aegean Sea</term><term>Crete</term><term>Dodecanese</term><term>Ionian Sea</term><term>Milos</term><term>Pixel</term><term>Space remote sensing</term><term>boreholes</term><term>digital elevation models</term><term>enthalpy</term><term>geothermal fields</term><term>granodiorites</term><term>imagery</term><term>interpretation</term><term>modern</term><term>plutons</term><term>satellites</term><term>spatial distribution</term><term>surface temperature</term><term>thermal anomalies</term><term>volcanic arcs</term><term>volcanoes</term></keywords><keywords scheme="Pascal" xml:lang="fr"><term>Champ géothermique</term><term>Actuel</term><term>Imagerie</term><term>Satellite</term><term>Température surface</term><term>Pixel</term><term>Modèle numérique élévation</term><term>Distribution spatiale</term><term>Arc volcanique</term><term>Enthalpie</term><term>Interprétation</term><term>Télédétection spatiale</term><term>Anomalie thermique</term><term>Volcan</term><term>Granodiorite</term><term>Pluton</term><term>Puits forage</term><term>Mer Ionienne</term><term>Crète</term><term>Ile Milos</term><term>Iles Dodécanèse</term><term>Mer Egée</term></keywords><keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Satellite</term><term>Interprétation</term><term>Mer Ionienne</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">The Hellenic Peninsula and the adjacent Aegean and Ionian seas are segmented into regions on the basis of Terra satellite-MODIS instrument derived land surface temperatures (LST) to test if they can be used in the field reconnaissance for potential geothermal targets, each region representing a different thermal signature. The method has been used successfully to identify hot spot and geothermal activity in the Afar Triangle and in the Red Sea. Night monthly average LST values per pixel, since 2001, are used in this work for geothermal field identification. Average LST seasonal variability is expressed by a common centroid curve of pixel cluster. Clusters were subsequently ranked in increasing LST according to their centroids. Cluster-2 represents by far the Aegean volcanic arc (AVA) which comprises the high enthalpy (320 and 350°C, respectively) geothermal fields of Milos and Nisyros. The interpretation of LST terrain segmentation into sub-clusters of Cluster-2 is consistent with thermal anomalies related to the volcano-islands of the AVA, the occurrence of thermal anomalies related to granodiorite plutons in the Cyclades and to the volcano-related anomalies of the Dodecanese Province. We conclude that the identification of such thermal anomalies obtained by a combination of remote sensing (LST), regional geology and field data (borehole, thermal spring and subsurface hydrothermal reservoir temperatures) can be a particularly useful exploration tool for localizing geothermal anomalies.</div></front></TEI><inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>1866-6280</s0></fA01><fA03 i2="1"><s0>Environ. earth sci. : (Print)</s0></fA03><fA05><s2>62</s2></fA05><fA06><s2>4</s2></fA06><fA08 i1="01" i2="1" l="ENG"><s1>Probable regional geothermal field reconnaissance in the Aegean region from modern multi-temporal night LST imagery</s1></fA08><fA11 i1="01" i2="1"><s1>ZOUZIAS (D.)</s1></fA11><fA11 i1="02" i2="1"><s1>MILIARESIS (George Ch.)</s1></fA11><fA11 i1="03" i2="1"><s1>SEYMOUR (K. St.)</s1></fA11><fA14 i1="01"><s1>Department of Geology, University of Patras</s1><s2>26504 Rion</s2><s3>GRC</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ></fA14><fA14 i1="02"><s1>Department of Geography, Urban Planning and Environment, Concordia University</s1><s2>Montreal, QC H3G1M8</s2><s3>CAN</s3><sZ>3 aut.</sZ></fA14><fA20><s1>717-723</s1></fA20><fA21><s1>2011</s1></fA21><fA23 i1="01"><s0>ENG</s0></fA23><fA43 i1="01"><s1>INIST</s1><s2>16770</s2><s5>354000194604690040</s5></fA43><fA44><s0>0000</s0><s1>© 2011 INIST-CNRS. All rights reserved.</s1></fA44><fA45><s0>1/2 p.</s0></fA45><fA47 i1="01" i2="1"><s0>11-0166701</s0></fA47><fA60><s1>P</s1></fA60><fA61><s0>A</s0></fA61><fA64 i1="01" i2="1"><s0>Environmental earth sciences : (Print)</s0></fA64><fA66 i1="01"><s0>DEU</s0></fA66><fC01 i1="01" l="ENG"><s0>The Hellenic Peninsula and the adjacent Aegean and Ionian seas are segmented into regions on the basis of Terra satellite-MODIS instrument derived land surface temperatures (LST) to test if they can be used in the field reconnaissance for potential geothermal targets, each region representing a different thermal signature. The method has been used successfully to identify hot spot and geothermal activity in the Afar Triangle and in the Red Sea. Night monthly average LST values per pixel, since 2001, are used in this work for geothermal field identification. Average LST seasonal variability is expressed by a common centroid curve of pixel cluster. Clusters were subsequently ranked in increasing LST according to their centroids. Cluster-2 represents by far the Aegean volcanic arc (AVA) which comprises the high enthalpy (320 and 350°C, respectively) geothermal fields of Milos and Nisyros. The interpretation of LST terrain segmentation into sub-clusters of Cluster-2 is consistent with thermal anomalies related to the volcano-islands of the AVA, the occurrence of thermal anomalies related to granodiorite plutons in the Cyclades and to the volcano-related anomalies of the Dodecanese Province. We conclude that the identification of such thermal anomalies obtained by a combination of remote sensing (LST), regional geology and field data (borehole, thermal spring and subsurface hydrothermal reservoir temperatures) can be a particularly useful exploration tool for localizing geothermal anomalies.</s0></fC01><fC02 i1="01" i2="2"><s0>001E01M04</s0></fC02><fC02 i1="02" i2="2"><s0>001E01O03</s0></fC02><fC02 i1="03" i2="2"><s0>225B04</s0></fC02><fC02 i1="04" i2="2"><s0>226B03</s0></fC02><fC03 i1="01" i2="2" l="FRE"><s0>Champ géothermique</s0><s5>01</s5></fC03><fC03 i1="01" i2="2" l="ENG"><s0>geothermal fields</s0><s5>01</s5></fC03><fC03 i1="01" i2="2" l="SPA"><s0>Campo geotérmico</s0><s5>01</s5></fC03><fC03 i1="02" i2="2" l="FRE"><s0>Actuel</s0><s5>02</s5></fC03><fC03 i1="02" i2="2" l="ENG"><s0>modern</s0><s5>02</s5></fC03><fC03 i1="02" i2="2" l="SPA"><s0>Actual</s0><s5>02</s5></fC03><fC03 i1="03" i2="2" l="FRE"><s0>Imagerie</s0><s5>03</s5></fC03><fC03 i1="03" i2="2" l="ENG"><s0>imagery</s0><s5>03</s5></fC03><fC03 i1="03" i2="2" l="SPA"><s0>Imaginería</s0><s5>03</s5></fC03><fC03 i1="04" i2="2" l="FRE"><s0>Satellite</s0><s5>04</s5></fC03><fC03 i1="04" i2="2" l="ENG"><s0>satellites</s0><s5>04</s5></fC03><fC03 i1="04" i2="2" l="SPA"><s0>Satélite</s0><s5>04</s5></fC03><fC03 i1="05" i2="2" l="FRE"><s0>Température surface</s0><s5>06</s5></fC03><fC03 i1="05" i2="2" l="ENG"><s0>surface temperature</s0><s5>06</s5></fC03><fC03 i1="06" i2="2" l="FRE"><s0>Pixel</s0><s5>10</s5></fC03><fC03 i1="06" i2="2" l="ENG"><s0>Pixel</s0><s5>10</s5></fC03><fC03 i1="06" i2="2" l="SPA"><s0>Pixel</s0><s5>10</s5></fC03><fC03 i1="07" i2="2" l="FRE"><s0>Modèle numérique élévation</s0><s5>11</s5></fC03><fC03 i1="07" i2="2" l="ENG"><s0>digital elevation models</s0><s5>11</s5></fC03><fC03 i1="08" i2="2" l="FRE"><s0>Distribution spatiale</s0><s5>12</s5></fC03><fC03 i1="08" i2="2" l="ENG"><s0>spatial distribution</s0><s5>12</s5></fC03><fC03 i1="08" i2="2" l="SPA"><s0>Distribución espacial</s0><s5>12</s5></fC03><fC03 i1="09" i2="2" l="FRE"><s0>Arc volcanique</s0><s5>13</s5></fC03><fC03 i1="09" i2="2" l="ENG"><s0>volcanic arcs</s0><s5>13</s5></fC03><fC03 i1="10" i2="2" l="FRE"><s0>Enthalpie</s0><s5>14</s5></fC03><fC03 i1="10" i2="2" l="ENG"><s0>enthalpy</s0><s5>14</s5></fC03><fC03 i1="10" i2="2" l="SPA"><s0>Entalpía</s0><s5>14</s5></fC03><fC03 i1="11" i2="2" l="FRE"><s0>Interprétation</s0><s5>15</s5></fC03><fC03 i1="11" i2="2" l="ENG"><s0>interpretation</s0><s5>15</s5></fC03><fC03 i1="11" i2="2" l="SPA"><s0>Interpretación</s0><s5>15</s5></fC03><fC03 i1="12" i2="2" l="FRE"><s0>Télédétection spatiale</s0><s5>16</s5></fC03><fC03 i1="12" i2="2" l="ENG"><s0>Space remote sensing</s0><s5>16</s5></fC03><fC03 i1="12" i2="2" l="SPA"><s0>Teledetección espacial</s0><s5>16</s5></fC03><fC03 i1="13" i2="2" l="FRE"><s0>Anomalie thermique</s0><s5>18</s5></fC03><fC03 i1="13" i2="2" l="ENG"><s0>thermal anomalies</s0><s5>18</s5></fC03><fC03 i1="13" i2="2" l="SPA"><s0>Anomalía termal</s0><s5>18</s5></fC03><fC03 i1="14" i2="2" l="FRE"><s0>Volcan</s0><s5>19</s5></fC03><fC03 i1="14" i2="2" l="ENG"><s0>volcanoes</s0><s5>19</s5></fC03><fC03 i1="14" i2="2" l="SPA"><s0>Volcán</s0><s5>19</s5></fC03><fC03 i1="15" i2="2" l="FRE"><s0>Granodiorite</s0><s2>NV</s2><s5>20</s5></fC03><fC03 i1="15" i2="2" l="ENG"><s0>granodiorites</s0><s2>NV</s2><s5>20</s5></fC03><fC03 i1="15" i2="2" l="SPA"><s0>Granodioritis</s0><s2>NV</s2><s5>20</s5></fC03><fC03 i1="16" i2="2" l="FRE"><s0>Pluton</s0><s5>21</s5></fC03><fC03 i1="16" i2="2" l="ENG"><s0>plutons</s0><s5>21</s5></fC03><fC03 i1="17" i2="2" l="FRE"><s0>Puits forage</s0><s5>23</s5></fC03><fC03 i1="17" i2="2" l="ENG"><s0>boreholes</s0><s5>23</s5></fC03><fC03 i1="18" i2="2" l="FRE"><s0>Mer Ionienne</s0><s2>NG</s2><s5>61</s5></fC03><fC03 i1="18" i2="2" l="ENG"><s0>Ionian Sea</s0><s2>NG</s2><s5>61</s5></fC03><fC03 i1="18" i2="2" l="SPA"><s0>Mar Jónico</s0><s2>NG</s2><s5>61</s5></fC03><fC03 i1="19" i2="2" l="FRE"><s0>Crète</s0><s2>NG</s2><s5>62</s5></fC03><fC03 i1="19" i2="2" l="ENG"><s0>Crete</s0><s2>NG</s2><s5>62</s5></fC03><fC03 i1="19" i2="2" l="SPA"><s0>Cresta</s0><s2>NG</s2><s5>62</s5></fC03><fC03 i1="20" i2="2" l="FRE"><s0>Ile Milos</s0><s2>NG</s2><s5>63</s5></fC03><fC03 i1="20" i2="2" l="ENG"><s0>Milos</s0><s2>NG</s2><s5>63</s5></fC03><fC03 i1="21" i2="2" l="FRE"><s0>Iles Dodécanèse</s0><s2>NG</s2><s5>65</s5></fC03><fC03 i1="21" i2="2" l="ENG"><s0>Dodecanese</s0><s2>NG</s2><s5>65</s5></fC03><fC03 i1="21" i2="2" l="SPA"><s0>Islas Dodecanese</s0><s2>NG</s2><s5>65</s5></fC03><fC03 i1="22" i2="2" l="FRE"><s0>Mer Egée</s0><s2>NG</s2><s5>66</s5></fC03><fC03 i1="22" i2="2" l="ENG"><s0>Aegean Sea</s0><s2>NG</s2><s5>66</s5></fC03><fC03 i1="22" i2="2" l="SPA"><s0>Mar Egeo</s0><s2>NG</s2><s5>66</s5></fC03><fC07 i1="01" i2="2" l="FRE"><s0>Roche plutonique</s0><s2>NV</s2></fC07><fC07 i1="01" i2="2" l="ENG"><s0>plutonic rocks</s0><s2>NV</s2></fC07><fC07 i1="01" i2="2" l="SPA"><s0>Roca granuda</s0><s2>NV</s2></fC07><fC07 i1="02" i2="2" l="FRE"><s0>Roche ignée</s0><s2>NV</s2></fC07><fC07 i1="02" i2="2" l="ENG"><s0>igneous rocks</s0><s2>NV</s2></fC07><fC07 i1="02" i2="2" l="SPA"><s0>Roca ignea</s0><s2>NV</s2></fC07><fC07 i1="03" i2="2" l="FRE"><s0>Mer Méditerranée Est</s0><s2>NG</s2></fC07><fC07 i1="03" i2="2" l="ENG"><s0>East Mediterranean</s0><s2>NG</s2></fC07><fC07 i1="03" i2="2" l="SPA"><s0>Mar Mediterraneo Este</s0><s2>NG</s2></fC07><fC07 i1="04" i2="2" l="FRE"><s0>Mer Méditerranée</s0><s2>564</s2></fC07><fC07 i1="04" i2="2" l="ENG"><s0>Mediterranean Sea</s0><s2>564</s2></fC07><fC07 i1="04" i2="2" l="SPA"><s0>Mar Mediterráneo</s0><s2>564</s2></fC07><fC07 i1="05" i2="2" l="FRE"><s0>Grèce</s0><s2>NG</s2></fC07><fC07 i1="05" i2="2" l="ENG"><s0>Greece</s0><s2>NG</s2></fC07><fC07 i1="05" i2="2" l="SPA"><s0>Grecia</s0><s2>NG</s2></fC07><fC07 i1="06" i2="2" l="FRE"><s0>Europe Sud</s0><s2>NG</s2></fC07><fC07 i1="06" i2="2" l="ENG"><s0>Southern Europe</s0><s2>NG</s2></fC07><fC07 i1="06" i2="2" l="SPA"><s0>Europa Sur</s0><s2>NG</s2></fC07><fC07 i1="07" i2="2" l="FRE"><s0>Europe</s0><s2>564</s2></fC07><fC07 i1="07" i2="2" l="ENG"><s0>Europe</s0><s2>564</s2></fC07><fC07 i1="07" i2="2" l="SPA"><s0>Europa</s0><s2>564</s2></fC07><fC07 i1="08" i2="2" l="FRE"><s0>Iles Cyclades</s0><s2>NG</s2></fC07><fC07 i1="08" i2="2" l="ENG"><s0>Cyclades</s0><s2>NG</s2></fC07><fC07 i1="08" i2="2" l="SPA"><s0>Islas Cyclades</s0><s2>NG</s2></fC07><fC07 i1="09" i2="2" l="FRE"><s0>Iles Egée Grèce</s0><s2>NG</s2></fC07><fC07 i1="09" i2="2" l="ENG"><s0>Greek Aegean Islands</s0><s2>NG</s2></fC07><fC07 i1="09" i2="2" l="SPA"><s0>Islas Egeas Griegas</s0><s2>NG</s2></fC07><fN21><s1>108</s1></fN21></pA></standard></inist><affiliations><list><country><li>Canada</li><li>Grèce</li></country></list><tree><country name="Grèce"><noRegion><name sortKey="Zouzias, D" sort="Zouzias, D" uniqKey="Zouzias D" first="D." last="Zouzias">D. Zouzias</name></noRegion><name sortKey="Miliaresis, George Ch" sort="Miliaresis, George Ch" uniqKey="Miliaresis G" first="George Ch." last="Miliaresis">George Ch. Miliaresis</name></country><country name="Canada"><noRegion><name sortKey="Seymour, K St" sort="Seymour, K St" uniqKey="Seymour K" first="K. St." last="Seymour">K. St. Seymour</name></noRegion></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
EXPLOR_STEP=$WICRI_ROOT/Wicri/Terre/explor/NissirosV1/Data/PascalFrancis/Checkpoint
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 000007 | SxmlIndent | more
Ou
HfdSelect -h $EXPLOR_AREA/Data/PascalFrancis/Checkpoint/biblio.hfd -nk 000007 | SxmlIndent | more
Pour mettre un lien sur cette page dans le réseau Wicri
{{Explor lien
|wiki= Wicri/Terre
|area= NissirosV1
|flux= PascalFrancis
|étape= Checkpoint
|type= RBID
|clé= Pascal:11-0166701
|texte= Probable regional geothermal field reconnaissance in the Aegean region from modern multi-temporal night LST imagery
}}
| This area was generated with Dilib version V0.6.33. |  |