Adakitic Paracale Granodiorite in southeastern Luzon, Philippines: A peek at a Proto-Philippine Sea Plate-related magmatic arc

This paper describes the geochemistry, petrogenesis and tectonic setting of a silicic pluton, the Paracale Granodiorite (PG), intruded into an ophiolitic suite in southeastern Luzon island, Philippines. Whole rock chemistry suggests that the PG samples are calc-alkaline and are characterized by ligh...

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Main Authors: Yumul, Graciano P, Jr, Queaño, Karlo L, Padrones, Jenielyn T, Dimalanta, Carla B, Andal, Eric A
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Published: Archīum Ateneo 2020
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Online Access:https://archium.ateneo.edu/es-faculty-pubs/63
https://archium.ateneo.edu/cgi/viewcontent.cgi?article=1062&context=es-faculty-pubs
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spelling ph-ateneo-arc.es-faculty-pubs-10622022-02-14T01:33:52Z Adakitic Paracale Granodiorite in southeastern Luzon, Philippines: A peek at a Proto-Philippine Sea Plate-related magmatic arc Yumul, Graciano P, Jr Queaño, Karlo L Padrones, Jenielyn T Dimalanta, Carla B Andal, Eric A This paper describes the geochemistry, petrogenesis and tectonic setting of a silicic pluton, the Paracale Granodiorite (PG), intruded into an ophiolitic suite in southeastern Luzon island, Philippines. Whole rock chemistry suggests that the PG samples are calc-alkaline and are characterized by light rare earth element (LREE)-enrichment and relatively weak heavy rare earth element (HREE)-depletion. They also show depletion in Nb, Ta, Zr and Ti and positive anomalies in K, Pb and Sr when normalized with the Primordial Mantle and normal-mid-ocean ridge basalt (N-MORB). The PG biotite mineral chemistry shows an affinity to calc-alkaline trends based on the FeOtot versus Al2O3, whereas in the MgO-Al2O3 plot, they exhibit transitional calc-alkaline to peraluminous characteristics. These information, along with a temperature >600 °C based on biotite chemistry, and hydrous setting for the generation of the PG suggest generation in a subduction-related setting. When plotted in the Y versus Sr/Y and YbN versus (La/Yb)N, the PG samples exhibit adakitic signature. Partial melting, fluid addition and sediment participation are discerned from the geochemistry. Melting, assimilation, storage and homogenization (MASH) with limited fractionation are the dominant mechanisms of formation. The PG could represent a Late Cretaceous to Paleogene magmatic arc generated during the subduction of the proto-Philippine Sea Plate. 2020-01-01T08:00:00Z text application/pdf https://archium.ateneo.edu/es-faculty-pubs/63 https://archium.ateneo.edu/cgi/viewcontent.cgi?article=1062&context=es-faculty-pubs Environmental Science Faculty Publications Archīum Ateneo Adakitic rock Paracale Granodiorite Subduction zone Proto-Philippine Sea Plate Environmental Sciences Natural Resources Management and Policy
institution Ateneo De Manila University
building Ateneo De Manila University Library
continent Asia
country Philippines
Philippines
content_provider Ateneo De Manila University Library
collection archium.Ateneo Institutional Repository
topic Adakitic rock
Paracale Granodiorite
Subduction zone
Proto-Philippine Sea Plate
Environmental Sciences
Natural Resources Management and Policy
spellingShingle Adakitic rock
Paracale Granodiorite
Subduction zone
Proto-Philippine Sea Plate
Environmental Sciences
Natural Resources Management and Policy
Yumul, Graciano P, Jr
Queaño, Karlo L
Padrones, Jenielyn T
Dimalanta, Carla B
Andal, Eric A
Adakitic Paracale Granodiorite in southeastern Luzon, Philippines: A peek at a Proto-Philippine Sea Plate-related magmatic arc
description This paper describes the geochemistry, petrogenesis and tectonic setting of a silicic pluton, the Paracale Granodiorite (PG), intruded into an ophiolitic suite in southeastern Luzon island, Philippines. Whole rock chemistry suggests that the PG samples are calc-alkaline and are characterized by light rare earth element (LREE)-enrichment and relatively weak heavy rare earth element (HREE)-depletion. They also show depletion in Nb, Ta, Zr and Ti and positive anomalies in K, Pb and Sr when normalized with the Primordial Mantle and normal-mid-ocean ridge basalt (N-MORB). The PG biotite mineral chemistry shows an affinity to calc-alkaline trends based on the FeOtot versus Al2O3, whereas in the MgO-Al2O3 plot, they exhibit transitional calc-alkaline to peraluminous characteristics. These information, along with a temperature >600 °C based on biotite chemistry, and hydrous setting for the generation of the PG suggest generation in a subduction-related setting. When plotted in the Y versus Sr/Y and YbN versus (La/Yb)N, the PG samples exhibit adakitic signature. Partial melting, fluid addition and sediment participation are discerned from the geochemistry. Melting, assimilation, storage and homogenization (MASH) with limited fractionation are the dominant mechanisms of formation. The PG could represent a Late Cretaceous to Paleogene magmatic arc generated during the subduction of the proto-Philippine Sea Plate.
format text
author Yumul, Graciano P, Jr
Queaño, Karlo L
Padrones, Jenielyn T
Dimalanta, Carla B
Andal, Eric A
author_facet Yumul, Graciano P, Jr
Queaño, Karlo L
Padrones, Jenielyn T
Dimalanta, Carla B
Andal, Eric A
author_sort Yumul, Graciano P, Jr
title Adakitic Paracale Granodiorite in southeastern Luzon, Philippines: A peek at a Proto-Philippine Sea Plate-related magmatic arc
title_short Adakitic Paracale Granodiorite in southeastern Luzon, Philippines: A peek at a Proto-Philippine Sea Plate-related magmatic arc
title_full Adakitic Paracale Granodiorite in southeastern Luzon, Philippines: A peek at a Proto-Philippine Sea Plate-related magmatic arc
title_fullStr Adakitic Paracale Granodiorite in southeastern Luzon, Philippines: A peek at a Proto-Philippine Sea Plate-related magmatic arc
title_full_unstemmed Adakitic Paracale Granodiorite in southeastern Luzon, Philippines: A peek at a Proto-Philippine Sea Plate-related magmatic arc
title_sort adakitic paracale granodiorite in southeastern luzon, philippines: a peek at a proto-philippine sea plate-related magmatic arc
publisher Archīum Ateneo
publishDate 2020
url https://archium.ateneo.edu/es-faculty-pubs/63
https://archium.ateneo.edu/cgi/viewcontent.cgi?article=1062&context=es-faculty-pubs
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