NissirosV1, PascalFrancis, Curation, bibRecord, 000029

Probable regional geothermal field reconnaissance in the Aegean region from modern multi-temporal night LST imagery

Identifieur interne : 000029 ( PascalFrancis/Curation ); précédent : 000028; suivant : 000030

Probable 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.

RBID : Pascal:11-0166701

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.

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A03		`1`		`@0 Environ. earth sci. : (Print)`
A05				`@2 62`
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A08	`01`	`1`	`ENG`	`@1 Probable regional geothermal field reconnaissance in the Aegean region from modern multi-temporal night LST imagery`
A11	`01`	`1`		`@1 ZOUZIAS (D.)`
A11	`02`	`1`		`@1 MILIARESIS (George Ch.)`
A11	`03`	`1`		`@1 SEYMOUR (K. St.)`
A14	`01`			`@1 Department of Geology, University of Patras @2 26504 Rion @3 GRC @Z 1 aut. @Z 2 aut.`
A14	`02`			`@1 Department of Geography, Urban Planning and Environment, Concordia University @2 Montreal, QC H3G1M8 @3 CAN @Z 3 aut.`
A20				`@1 717-723`
A21				`@1 2011`
A23	`01`			`@0 ENG`
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A44				`@0 0000 @1 © 2011 INIST-CNRS. All rights reserved.`
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C01	`01`		`ENG`	@0 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.
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C03	`01`	`2`	`FRE`	`@0 Champ géothermique @5 01`
C03	`01`	`2`	`ENG`	`@0 geothermal fields @5 01`
C03	`01`	`2`	`SPA`	`@0 Campo geotérmico @5 01`
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C03	`03`	`2`	`SPA`	`@0 Imaginería @5 03`
C03	`04`	`2`	`FRE`	`@0 Satellite @5 04`
C03	`04`	`2`	`ENG`	`@0 satellites @5 04`
C03	`04`	`2`	`SPA`	`@0 Satélite @5 04`
C03	`05`	`2`	`FRE`	`@0 Température surface @5 06`
C03	`05`	`2`	`ENG`	`@0 surface temperature @5 06`
C03	`06`	`2`	`FRE`	`@0 Pixel @5 10`
C03	`06`	`2`	`ENG`	`@0 Pixel @5 10`
C03	`06`	`2`	`SPA`	`@0 Pixel @5 10`
C03	`07`	`2`	`FRE`	`@0 Modèle numérique élévation @5 11`
C03	`07`	`2`	`ENG`	`@0 digital elevation models @5 11`
C03	`08`	`2`	`FRE`	`@0 Distribution spatiale @5 12`
C03	`08`	`2`	`ENG`	`@0 spatial distribution @5 12`
C03	`08`	`2`	`SPA`	`@0 Distribución espacial @5 12`
C03	`09`	`2`	`FRE`	`@0 Arc volcanique @5 13`
C03	`09`	`2`	`ENG`	`@0 volcanic arcs @5 13`
C03	`10`	`2`	`FRE`	`@0 Enthalpie @5 14`
C03	`10`	`2`	`ENG`	`@0 enthalpy @5 14`
C03	`10`	`2`	`SPA`	`@0 Entalpía @5 14`
C03	`11`	`2`	`FRE`	`@0 Interprétation @5 15`
C03	`11`	`2`	`ENG`	`@0 interpretation @5 15`
C03	`11`	`2`	`SPA`	`@0 Interpretación @5 15`
C03	`12`	`2`	`FRE`	`@0 Télédétection spatiale @5 16`
C03	`12`	`2`	`ENG`	`@0 Space remote sensing @5 16`
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C03	`13`	`2`	`FRE`	`@0 Anomalie thermique @5 18`
C03	`13`	`2`	`ENG`	`@0 thermal anomalies @5 18`
C03	`13`	`2`	`SPA`	`@0 Anomalía termal @5 18`
C03	`14`	`2`	`FRE`	`@0 Volcan @5 19`
C03	`14`	`2`	`ENG`	`@0 volcanoes @5 19`
C03	`14`	`2`	`SPA`	`@0 Volcán @5 19`
C03	`15`	`2`	`FRE`	`@0 Granodiorite @2 NV @5 20`
C03	`15`	`2`	`ENG`	`@0 granodiorites @2 NV @5 20`
C03	`15`	`2`	`SPA`	`@0 Granodioritis @2 NV @5 20`
C03	`16`	`2`	`FRE`	`@0 Pluton @5 21`
C03	`16`	`2`	`ENG`	`@0 plutons @5 21`
C03	`17`	`2`	`FRE`	`@0 Puits forage @5 23`
C03	`17`	`2`	`ENG`	`@0 boreholes @5 23`
C03	`18`	`2`	`FRE`	`@0 Mer Ionienne @2 NG @5 61`
C03	`18`	`2`	`ENG`	`@0 Ionian Sea @2 NG @5 61`
C03	`18`	`2`	`SPA`	`@0 Mar Jónico @2 NG @5 61`
C03	`19`	`2`	`FRE`	`@0 Crète @2 NG @5 62`
C03	`19`	`2`	`ENG`	`@0 Crete @2 NG @5 62`
C03	`19`	`2`	`SPA`	`@0 Cresta @2 NG @5 62`
C03	`20`	`2`	`FRE`	`@0 Ile Milos @2 NG @5 63`
C03	`20`	`2`	`ENG`	`@0 Milos @2 NG @5 63`
C03	`21`	`2`	`FRE`	`@0 Iles Dodécanèse @2 NG @5 65`
C03	`21`	`2`	`ENG`	`@0 Dodecanese @2 NG @5 65`
C03	`21`	`2`	`SPA`	`@0 Islas Dodecanese @2 NG @5 65`
C03	`22`	`2`	`FRE`	`@0 Mer Egée @2 NG @5 66`
C03	`22`	`2`	`ENG`	`@0 Aegean Sea @2 NG @5 66`
C03	`22`	`2`	`SPA`	`@0 Mar Egeo @2 NG @5 66`
C07	`01`	`2`	`FRE`	`@0 Roche plutonique @2 NV`
C07	`01`	`2`	`ENG`	`@0 plutonic rocks @2 NV`
C07	`01`	`2`	`SPA`	`@0 Roca granuda @2 NV`
C07	`02`	`2`	`FRE`	`@0 Roche ignée @2 NV`
C07	`02`	`2`	`ENG`	`@0 igneous rocks @2 NV`
C07	`02`	`2`	`SPA`	`@0 Roca ignea @2 NV`
C07	`03`	`2`	`FRE`	`@0 Mer Méditerranée Est @2 NG`
C07	`03`	`2`	`ENG`	`@0 East Mediterranean @2 NG`
C07	`03`	`2`	`SPA`	`@0 Mar Mediterraneo Este @2 NG`
C07	`04`	`2`	`FRE`	`@0 Mer Méditerranée @2 564`
C07	`04`	`2`	`ENG`	`@0 Mediterranean Sea @2 564`
C07	`04`	`2`	`SPA`	`@0 Mar Mediterráneo @2 564`
C07	`05`	`2`	`FRE`	`@0 Grèce @2 NG`
C07	`05`	`2`	`ENG`	`@0 Greece @2 NG`
C07	`05`	`2`	`SPA`	`@0 Grecia @2 NG`
C07	`06`	`2`	`FRE`	`@0 Europe Sud @2 NG`
C07	`06`	`2`	`ENG`	`@0 Southern Europe @2 NG`
C07	`06`	`2`	`SPA`	`@0 Europa Sur @2 NG`
C07	`07`	`2`	`FRE`	`@0 Europe @2 564`
C07	`07`	`2`	`ENG`	`@0 Europe @2 564`
C07	`07`	`2`	`SPA`	`@0 Europa @2 564`
C07	`08`	`2`	`FRE`	`@0 Iles Cyclades @2 NG`
C07	`08`	`2`	`ENG`	`@0 Cyclades @2 NG`
C07	`08`	`2`	`SPA`	`@0 Islas Cyclades @2 NG`
C07	`09`	`2`	`FRE`	`@0 Iles Egée Grèce @2 NG`
C07	`09`	`2`	`ENG`	`@0 Greek Aegean Islands @2 NG`
C07	`09`	`2`	`SPA`	`@0 Islas Egeas Griegas @2 NG`
N21				`@1 108`

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Le document en format XML

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<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>
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<term>spatial distribution</term>
<term>surface temperature</term>
<term>thermal anomalies</term>
<term>volcanic arcs</term>
<term>volcanoes</term>
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<keywords scheme="Pascal" xml:lang="fr"><term>Champ géothermique</term>
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<term>Imagerie</term>
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<term>Pixel</term>
<term>Modèle numérique élévation</term>
<term>Distribution spatiale</term>
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<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>
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<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>
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<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>
</record>

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   |texte=   Probable regional geothermal field reconnaissance in the Aegean region from modern multi-temporal night LST imagery
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Probable regional geothermal field reconnaissance in the Aegean region from modern multi-temporal night LST imagery

Probable regional geothermal field reconnaissance in the Aegean region from modern multi-temporal night LST imagery

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