Ancellin, Marie-Anne, Vlastélic, Ivan, Samaniego, Pablo, Nauret, François, Gannoun, Abdelmouhcine, Hidalgo, Silvana (2019) Up to 1% Pb isotope disequilibrium between minerals hosted in dacites from the Guagua Pichincha volcano, Ecuador: Implication for tracing the source and crustal history of continental arc magmas. Chemical Geology, 525. 177-189 doi:10.1016/j.chemgeo.2019.07.016

| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Up to 1% Pb isotope disequilibrium between minerals hosted in dacites from the Guagua Pichincha volcano, Ecuador: Implication for tracing the source and crustal history of continental arc magmas | ||
| Journal | Chemical Geology | ||
| Authors | Ancellin, Marie-Anne | Author | |
| Vlastélic, Ivan | Author | ||
| Samaniego, Pablo | Author | ||
| Nauret, François | Author | ||
| Gannoun, Abdelmouhcine | Author | ||
| Hidalgo, Silvana | Author | ||
| Year | 2019 (October) | Volume | 525 |
| Publisher | Elsevier BV | ||
| DOI | doi:10.1016/j.chemgeo.2019.07.016Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 300282 | Long-form Identifier | mindat:1:5:300282:1 |
| GUID | 0 | ||
| Full Reference | Ancellin, Marie-Anne, Vlastélic, Ivan, Samaniego, Pablo, Nauret, François, Gannoun, Abdelmouhcine, Hidalgo, Silvana (2019) Up to 1% Pb isotope disequilibrium between minerals hosted in dacites from the Guagua Pichincha volcano, Ecuador: Implication for tracing the source and crustal history of continental arc magmas. Chemical Geology, 525. 177-189 doi:10.1016/j.chemgeo.2019.07.016 | ||
| Plain Text | Ancellin, Marie-Anne, Vlastélic, Ivan, Samaniego, Pablo, Nauret, François, Gannoun, Abdelmouhcine, Hidalgo, Silvana (2019) Up to 1% Pb isotope disequilibrium between minerals hosted in dacites from the Guagua Pichincha volcano, Ecuador: Implication for tracing the source and crustal history of continental arc magmas. Chemical Geology, 525. 177-189 doi:10.1016/j.chemgeo.2019.07.016 | ||
| In | (2019) Chemical Geology Vol. 525. Elsevier BV | ||
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