Noble gas and boron isotopic signatures of the Bacon-Manito geothermal fluid, Philippines. (Articolo in rivista)

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  • Noble gas and boron isotopic signatures of the Bacon-Manito geothermal fluid, Philippines. (Articolo in rivista) (literal)
Anno
  • 2008-01-01T00:00:00+01:00 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
  • 10.1111/j.1468-8123.2008.00224.x (literal)
Alternative label
  • Bayon F.E.B. (1); See F.S. (1); Magro G.; (2); Pennisi M. (2) (2008)
    Noble gas and boron isotopic signatures of the Bacon-Manito geothermal fluid, Philippines.
    in Geofluids (Oxford. Print); Wiley-Blackwell Publishing, Inc., Malden (Stati Uniti d'America)
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Bayon F.E.B. (1); See F.S. (1); Magro G.; (2); Pennisi M. (2) (literal)
Pagina inizio
  • 230 (literal)
Pagina fine
  • 238 (literal)
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  • This work represents the fruit of a technical cooperation project with the International Atomic Energy Agency (IAEA; PHI- 8/ 023). (literal)
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  • 8 (literal)
Rivista
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  • 4 (literal)
Note
  • ISI Web of Science (WOS) (literal)
  • Scopu (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • 1. Energy Dev Corp, Taguig, Philippines 2. CNR, Ist Geosci & Georisorse, I-56100 Pisa, Italy (literal)
Titolo
  • Noble gas and boron isotopic signatures of the Bacon-Manito geothermal fluid, Philippines. (literal)
Abstract
  • Noble gas isotopic composition and abundances were determined on dry gas sampled in geothermal wells from the Bacon-Manito (BGPF) geothermal field in the Philippines. The most significant findings come from the (3)He/(4)He ratio; a mantle-He source is evidenced by ratio close to 7 Ra. Peripheral fluid from the west and south of the geothermal system is relatively enriched in (4)He (R/Ra slightly > 2), most probably sourced from U and Th decay in old igneous or crustal rocks. The two end-members mix, producing the range of R/Ra ratios observed in the other wells included in this study. Preliminary data on the delta(11)B signature of the Bacon Manito fluid separated from vapour range from 7 parts per thousand to 9 parts per thousand. These values suggest that the local magmatic rocks could represent the main boron source, in agreement with the boron isotopic signature of Pacific arc lavas. (literal)
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