Alteration processes recorded by back‐arc mantle peridotites from oceanic core complexes, Shikoku Basin, Philippine Sea
We determined the mineralogical and petrological characteristics of ultramafic rocks dredged from two oceanic core complexes: the Mado Megamullion and 23°30′N non‐transform offset massif, which are located within the Shikoku back‐arc basin in the Philippine Sea. The ultramafic rocks are strongly ser...
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| Published in | The island arc Vol. 30; no. 1 |
|---|---|
| Main Authors | , , , , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Melbourne
John Wiley & Sons Australia, Ltd
01.01.2021
Wiley Subscription Services, Inc |
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| Abstract | We determined the mineralogical and petrological characteristics of ultramafic rocks dredged from two oceanic core complexes: the Mado Megamullion and 23°30′N non‐transform offset massif, which are located within the Shikoku back‐arc basin in the Philippine Sea. The ultramafic rocks are strongly serpentinized, but can be classified as harzburgite/lherzolite or dunite, based on relict primary minerals and their pseudomorphs. Strongly elongated pyroxene porphyroclasts with undulatory extinction indicate high‐temperature (≥700 °C) strain localization on a detachment fault within the upper mantle at depths below the brittle–viscous transition. During exhumation, the peridotites underwent impregnation by magmatic or hydrothermal fluids, lizardite/chrysotile serpentinization at ≤300 °C, antigorite crystallization, and silica metasomatism that formed talc. These features indicate that the detachment fault zones formed a fluid pathway and facilitated a range of fluid–peridotite interactions. |
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| AbstractList | We determined the mineralogical and petrological characteristics of ultramafic rocks dredged from two oceanic core complexes: the Mado Megamullion and 23°30′N non‐transform offset massif, which are located within the Shikoku back‐arc basin in the Philippine Sea. The ultramafic rocks are strongly serpentinized, but can be classified as harzburgite/lherzolite or dunite, based on relict primary minerals and their pseudomorphs. Strongly elongated pyroxene porphyroclasts with undulatory extinction indicate high‐temperature (≥700 °C) strain localization on a detachment fault within the upper mantle at depths below the brittle–viscous transition. During exhumation, the peridotites underwent impregnation by magmatic or hydrothermal fluids, lizardite/chrysotile serpentinization at ≤300 °C, antigorite crystallization, and silica metasomatism that formed talc. These features indicate that the detachment fault zones formed a fluid pathway and facilitated a range of fluid–peridotite interactions. Abstract We determined the mineralogical and petrological characteristics of ultramafic rocks dredged from two oceanic core complexes: the Mado Megamullion and 23°30′N non‐transform offset massif, which are located within the Shikoku back‐arc basin in the Philippine Sea. The ultramafic rocks are strongly serpentinized, but can be classified as harzburgite/lherzolite or dunite, based on relict primary minerals and their pseudomorphs. Strongly elongated pyroxene porphyroclasts with undulatory extinction indicate high‐temperature (≥700 °C) strain localization on a detachment fault within the upper mantle at depths below the brittle–viscous transition. During exhumation, the peridotites underwent impregnation by magmatic or hydrothermal fluids, lizardite/chrysotile serpentinization at ≤300 °C, antigorite crystallization, and silica metasomatism that formed talc. These features indicate that the detachment fault zones formed a fluid pathway and facilitated a range of fluid–peridotite interactions. |
| Author | Sen, Atlanta Segawa, Izumi Ohara, Yasuhiko Fujii, Masakazu Hirauchi, Ken‐ichi Snow, Jonathan Kouketsu, Yui Harigane, Yumiko Okino, Kyoko |
| Author_xml | – sequence: 1 givenname: Ken‐ichi orcidid: 0000-0002-5318-4646 surname: Hirauchi fullname: Hirauchi, Ken‐ichi email: hirauchi.kenichi@shizuoka.ac.jp organization: Shizuoka University – sequence: 2 givenname: Izumi orcidid: 0000-0002-7704-7275 surname: Segawa fullname: Segawa, Izumi organization: Shizuoka University – sequence: 3 givenname: Yui orcidid: 0000-0001-8711-5457 surname: Kouketsu fullname: Kouketsu, Yui organization: Nagoya University – sequence: 4 givenname: Yumiko orcidid: 0000-0002-8133-0700 surname: Harigane fullname: Harigane, Yumiko organization: National Institute of Advanced Industrial Science and Technology (AIST) – sequence: 5 givenname: Yasuhiko orcidid: 0000-0002-9567-0802 surname: Ohara fullname: Ohara, Yasuhiko organization: Japan Agency for Marine‐Earth Science and Technology (JAMSTEC) – sequence: 6 givenname: Jonathan orcidid: 0000-0003-4244-7700 surname: Snow fullname: Snow, Jonathan organization: Louisiana State University – sequence: 7 givenname: Atlanta orcidid: 0000-0001-9232-5088 surname: Sen fullname: Sen, Atlanta organization: University of Houston – sequence: 8 givenname: Masakazu orcidid: 0000-0003-0527-1742 surname: Fujii fullname: Fujii, Masakazu organization: Geoscience Group – sequence: 9 givenname: Kyoko orcidid: 0000-0001-7070-7982 surname: Okino fullname: Okino, Kyoko organization: The University of Tokyo |
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| Snippet | We determined the mineralogical and petrological characteristics of ultramafic rocks dredged from two oceanic core complexes: the Mado Megamullion and 23°30′N... Abstract We determined the mineralogical and petrological characteristics of ultramafic rocks dredged from two oceanic core complexes: the Mado Megamullion and... |
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| SubjectTerms | back‐arc basin Chrysotile Crystallization Crystals detachment fault Dredging Ductile-brittle transition Dunite Fault zones Faults Fluids Localization Mado Megamullion Massifs Minerals oceanic core complex Peridotite Rocks serpentinite Serpentinization Shikoku Basin Silica Silicon dioxide Strain localization Ultramafic materials Ultramafic rocks Upper mantle |
| Title | Alteration processes recorded by back‐arc mantle peridotites from oceanic core complexes, Shikoku Basin, Philippine Sea |
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