Cap rock efficiency and fluid circulation of natural hydrothermal systems by means of XRD on clay minerals (Sutri, Northern Latium, Italy)
•We perform X-ray diffraction on cap rocks of a Northern Latium geothermal system.•Cap rock effectiveness and degree of interaction with hot fluids are detected.•Unfractured cap rock shows paleo-T
Gespeichert in:
| Veröffentlicht in: | Geothermics 2014-04, Vol.50, p.180-188 |
|---|---|
| Hauptverfasser: | , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 188 |
|---|---|
| container_issue | |
| container_start_page | 180 |
| container_title | Geothermics |
| container_volume | 50 |
| creator | Corrado, Sveva Aldega, Luca Celano, Antonio Stefano De Benedetti, Arnaldo Angelo Giordano, Guido |
| description | •We perform X-ray diffraction on cap rocks of a Northern Latium geothermal system.•Cap rock effectiveness and degree of interaction with hot fluids are detected.•Unfractured cap rock shows paleo-T |
| doi_str_mv | 10.1016/j.geothermics.2013.09.011 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_1506381022</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S0375650513000850</els_id><sourcerecordid>1506381022</sourcerecordid><originalsourceid>FETCH-LOGICAL-a407t-13f5c99a2c13b66a4c65074337ee8fdf62776281f43574fa9faf9edf258315a83</originalsourceid><addsrcrecordid>eNqNkV-L1DAUxYMoOK5-h_ggrLDtJk3TtI8yurowKPgHfAt30xs3Y5uMSbrQr7Cf2oyziI8-hYTfOfeeE0JeclZzxrvLff0DQ77FODuT6oZxUbOhZpw_Ihveq6ESUnWPyYYJJatOMvmUPEtpzxhTUrENud_CgcZgflK01hmH3qwU_EjttLiRGhfNMkF2wdNgqYe8RJjo7TrG09RySWvKOCd6s9IZwacj-P3zW1okZoLy6DwWUaLnX5Yc3QX9GOJR6-muGC_zBb3OMK2vn5MntmD44uE8I9-u3n3dfqh2n95fb9_sKmiZyhUXVpphgMZwcdN10JoSS7VCKMTejrZrlOqantu2RG8tDBbsgKNtZC-4hF6ckfOT7yGGXwumrGeXDE4TeAxL0lyyTvScNU1BhxNqYkgpotWH6GaIq-ZMH_vXe_1P__rYv2aDLv0X7auHMZAMTDaCNy79NSgbCiZEW7jticOS-c5h1OnPN-DoIpqsx-D-Y9pvj4Wi9A</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1506381022</pqid></control><display><type>article</type><title>Cap rock efficiency and fluid circulation of natural hydrothermal systems by means of XRD on clay minerals (Sutri, Northern Latium, Italy)</title><source>ScienceDirect Journals (5 years ago - present)</source><creator>Corrado, Sveva ; Aldega, Luca ; Celano, Antonio Stefano ; De Benedetti, Arnaldo Angelo ; Giordano, Guido</creator><creatorcontrib>Corrado, Sveva ; Aldega, Luca ; Celano, Antonio Stefano ; De Benedetti, Arnaldo Angelo ; Giordano, Guido</creatorcontrib><description>•We perform X-ray diffraction on cap rocks of a Northern Latium geothermal system.•Cap rock effectiveness and degree of interaction with hot fluids are detected.•Unfractured cap rock shows paleo-T <50–60°C and good insulation.•Fractured cap rock shows higher paleo-T (85–110°C) and interaction with hot fluids.
We performed XRD investigations on the sedimentary cap rock of the geothermal system developed in the area of Vico volcano (Northern Latium) to assess its effectiveness and degree of interaction with fluids. The system consists of a positive thermal anomaly, a permeable carbonate reservoir at shallow depths and a low permeability siliciclastic cap rock. Unfractured cap rock shows maximum paleo-temperatures <50–60°C, interpreted as the thermal signature of the original sedimentary basin. Fractured cap rock is characterized by kaolinite, calcite, short-range ordered mixed layers illite-smectite with paleo-temperatures between 85 and 110°C indicating strong interaction with hot fluids from a carbonate reservoir.</description><identifier>ISSN: 0375-6505</identifier><identifier>EISSN: 1879-3576</identifier><identifier>DOI: 10.1016/j.geothermics.2013.09.011</identifier><identifier>CODEN: GTMCAT</identifier><language>eng</language><publisher>Oxford: Elsevier Ltd</publisher><subject>Calcite ; Cap-rock ; Carbonates ; Earth sciences ; Earth, ocean, space ; Engineering and environment geology. Geothermics ; Exact sciences and technology ; Fluid dynamics ; Fluid flow ; Fluids ; Geothermics ; Italy ; Mixed layers illite-smectite ; Northern Latium ; Reservoirs ; Rock ; Thermal alteration ; Volcanoes ; X-ray diffraction</subject><ispartof>Geothermics, 2014-04, Vol.50, p.180-188</ispartof><rights>2013 Elsevier Ltd</rights><rights>2015 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a407t-13f5c99a2c13b66a4c65074337ee8fdf62776281f43574fa9faf9edf258315a83</citedby><cites>FETCH-LOGICAL-a407t-13f5c99a2c13b66a4c65074337ee8fdf62776281f43574fa9faf9edf258315a83</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.geothermics.2013.09.011$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,780,784,3548,27922,27923,45993</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=28130334$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Corrado, Sveva</creatorcontrib><creatorcontrib>Aldega, Luca</creatorcontrib><creatorcontrib>Celano, Antonio Stefano</creatorcontrib><creatorcontrib>De Benedetti, Arnaldo Angelo</creatorcontrib><creatorcontrib>Giordano, Guido</creatorcontrib><title>Cap rock efficiency and fluid circulation of natural hydrothermal systems by means of XRD on clay minerals (Sutri, Northern Latium, Italy)</title><title>Geothermics</title><description>•We perform X-ray diffraction on cap rocks of a Northern Latium geothermal system.•Cap rock effectiveness and degree of interaction with hot fluids are detected.•Unfractured cap rock shows paleo-T <50–60°C and good insulation.•Fractured cap rock shows higher paleo-T (85–110°C) and interaction with hot fluids.
We performed XRD investigations on the sedimentary cap rock of the geothermal system developed in the area of Vico volcano (Northern Latium) to assess its effectiveness and degree of interaction with fluids. The system consists of a positive thermal anomaly, a permeable carbonate reservoir at shallow depths and a low permeability siliciclastic cap rock. Unfractured cap rock shows maximum paleo-temperatures <50–60°C, interpreted as the thermal signature of the original sedimentary basin. Fractured cap rock is characterized by kaolinite, calcite, short-range ordered mixed layers illite-smectite with paleo-temperatures between 85 and 110°C indicating strong interaction with hot fluids from a carbonate reservoir.</description><subject>Calcite</subject><subject>Cap-rock</subject><subject>Carbonates</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Engineering and environment geology. Geothermics</subject><subject>Exact sciences and technology</subject><subject>Fluid dynamics</subject><subject>Fluid flow</subject><subject>Fluids</subject><subject>Geothermics</subject><subject>Italy</subject><subject>Mixed layers illite-smectite</subject><subject>Northern Latium</subject><subject>Reservoirs</subject><subject>Rock</subject><subject>Thermal alteration</subject><subject>Volcanoes</subject><subject>X-ray diffraction</subject><issn>0375-6505</issn><issn>1879-3576</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><recordid>eNqNkV-L1DAUxYMoOK5-h_ggrLDtJk3TtI8yurowKPgHfAt30xs3Y5uMSbrQr7Cf2oyziI8-hYTfOfeeE0JeclZzxrvLff0DQ77FODuT6oZxUbOhZpw_Ihveq6ESUnWPyYYJJatOMvmUPEtpzxhTUrENud_CgcZgflK01hmH3qwU_EjttLiRGhfNMkF2wdNgqYe8RJjo7TrG09RySWvKOCd6s9IZwacj-P3zW1okZoLy6DwWUaLnX5Yc3QX9GOJR6-muGC_zBb3OMK2vn5MntmD44uE8I9-u3n3dfqh2n95fb9_sKmiZyhUXVpphgMZwcdN10JoSS7VCKMTejrZrlOqantu2RG8tDBbsgKNtZC-4hF6ckfOT7yGGXwumrGeXDE4TeAxL0lyyTvScNU1BhxNqYkgpotWH6GaIq-ZMH_vXe_1P__rYv2aDLv0X7auHMZAMTDaCNy79NSgbCiZEW7jticOS-c5h1OnPN-DoIpqsx-D-Y9pvj4Wi9A</recordid><startdate>20140401</startdate><enddate>20140401</enddate><creator>Corrado, Sveva</creator><creator>Aldega, Luca</creator><creator>Celano, Antonio Stefano</creator><creator>De Benedetti, Arnaldo Angelo</creator><creator>Giordano, Guido</creator><general>Elsevier Ltd</general><general>Elsevier</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope></search><sort><creationdate>20140401</creationdate><title>Cap rock efficiency and fluid circulation of natural hydrothermal systems by means of XRD on clay minerals (Sutri, Northern Latium, Italy)</title><author>Corrado, Sveva ; Aldega, Luca ; Celano, Antonio Stefano ; De Benedetti, Arnaldo Angelo ; Giordano, Guido</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a407t-13f5c99a2c13b66a4c65074337ee8fdf62776281f43574fa9faf9edf258315a83</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2014</creationdate><topic>Calcite</topic><topic>Cap-rock</topic><topic>Carbonates</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Engineering and environment geology. Geothermics</topic><topic>Exact sciences and technology</topic><topic>Fluid dynamics</topic><topic>Fluid flow</topic><topic>Fluids</topic><topic>Geothermics</topic><topic>Italy</topic><topic>Mixed layers illite-smectite</topic><topic>Northern Latium</topic><topic>Reservoirs</topic><topic>Rock</topic><topic>Thermal alteration</topic><topic>Volcanoes</topic><topic>X-ray diffraction</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Corrado, Sveva</creatorcontrib><creatorcontrib>Aldega, Luca</creatorcontrib><creatorcontrib>Celano, Antonio Stefano</creatorcontrib><creatorcontrib>De Benedetti, Arnaldo Angelo</creatorcontrib><creatorcontrib>Giordano, Guido</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><jtitle>Geothermics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Corrado, Sveva</au><au>Aldega, Luca</au><au>Celano, Antonio Stefano</au><au>De Benedetti, Arnaldo Angelo</au><au>Giordano, Guido</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Cap rock efficiency and fluid circulation of natural hydrothermal systems by means of XRD on clay minerals (Sutri, Northern Latium, Italy)</atitle><jtitle>Geothermics</jtitle><date>2014-04-01</date><risdate>2014</risdate><volume>50</volume><spage>180</spage><epage>188</epage><pages>180-188</pages><issn>0375-6505</issn><eissn>1879-3576</eissn><coden>GTMCAT</coden><abstract>•We perform X-ray diffraction on cap rocks of a Northern Latium geothermal system.•Cap rock effectiveness and degree of interaction with hot fluids are detected.•Unfractured cap rock shows paleo-T <50–60°C and good insulation.•Fractured cap rock shows higher paleo-T (85–110°C) and interaction with hot fluids.
We performed XRD investigations on the sedimentary cap rock of the geothermal system developed in the area of Vico volcano (Northern Latium) to assess its effectiveness and degree of interaction with fluids. The system consists of a positive thermal anomaly, a permeable carbonate reservoir at shallow depths and a low permeability siliciclastic cap rock. Unfractured cap rock shows maximum paleo-temperatures <50–60°C, interpreted as the thermal signature of the original sedimentary basin. Fractured cap rock is characterized by kaolinite, calcite, short-range ordered mixed layers illite-smectite with paleo-temperatures between 85 and 110°C indicating strong interaction with hot fluids from a carbonate reservoir.</abstract><cop>Oxford</cop><pub>Elsevier Ltd</pub><doi>10.1016/j.geothermics.2013.09.011</doi><tpages>9</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0375-6505 |
| ispartof | Geothermics, 2014-04, Vol.50, p.180-188 |
| issn | 0375-6505 1879-3576 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_1506381022 |
| source | ScienceDirect Journals (5 years ago - present) |
| subjects | Calcite Cap-rock Carbonates Earth sciences Earth, ocean, space Engineering and environment geology. Geothermics Exact sciences and technology Fluid dynamics Fluid flow Fluids Geothermics Italy Mixed layers illite-smectite Northern Latium Reservoirs Rock Thermal alteration Volcanoes X-ray diffraction |
| title | Cap rock efficiency and fluid circulation of natural hydrothermal systems by means of XRD on clay minerals (Sutri, Northern Latium, Italy) |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-10T03%3A55%3A09IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Cap%20rock%20efficiency%20and%20fluid%20circulation%20of%20natural%20hydrothermal%20systems%20by%20means%20of%20XRD%20on%20clay%20minerals%20(Sutri,%20Northern%20Latium,%20Italy)&rft.jtitle=Geothermics&rft.au=Corrado,%20Sveva&rft.date=2014-04-01&rft.volume=50&rft.spage=180&rft.epage=188&rft.pages=180-188&rft.issn=0375-6505&rft.eissn=1879-3576&rft.coden=GTMCAT&rft_id=info:doi/10.1016/j.geothermics.2013.09.011&rft_dat=%3Cproquest_cross%3E1506381022%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1506381022&rft_id=info:pmid/&rft_els_id=S0375650513000850&rfr_iscdi=true |