Listvenite formation during mass transfer into the leading edge of the mantle wedge: initial results from Oman Drilling Project Hole BT1B
Listvenite formation during mass transfer into the leading edge of the mantle wedge: initial results from Oman Drilling Project Hole BT1B
This paper provides an overview of research on core from Oman Drilling Project Hole BT1B and the surrounding area, plus new data and calculations, constraining processes in the Tethyan subduction zone beneath the Samail ophiolite. The area is underlain by gently dipping, broadly folded layers of allochthonous Hawasina pelagic sediments, the metamorphic sole of the Samail ophiolite, and Banded Unit peridotites at the base of the Samail mantle section. Despite reactivation of some faults during uplift of the Jebel Akdar and Saih Hatat domes, the area preserves the tectonic “stratigraphy” of the Cretaceous subduction zone. Gently dipping listvenite bands, parallel to peridotite banding and to contacts between the peridotite and the metamorphic sole, replace peridotite at and near the basal thrust. Listvenites formed at less than 200°C and (poorly constrained) depths of 25–40 km by reaction with CO2-rich, aqueous fluids migrating from greater depths, derived from devolatilization of subducting sediments analogous to clastic sediments in the Hawasina Formation, at 400°–500°. Such processes could form important reservoirs for subducted CO2. Listvenite formation was accompanied by ductile deformation of serpentinites and listvenites—perhaps facilitated by fluid-rock reaction—in a process that could lead to aseismic subduction in some regions. Addition of H2O and CO2 to the mantle wedge, forming serpentinites and listvenites, caused large increases in the solid mass and volume of the rocks. This may have been accommodated by fractures formed as a result of volume changes, mainly at a serpentinization front.
Oman, Samail ophiolite, carbon cycle, ductile deformation, listvenite, subduction
Kelemen, Peter B.
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Carlos De Obeso, Juan
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Leong, James A.
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Godard, Marguerite
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Okazaki, Keishi
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Kotowski, Alissa J.
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Manning, Craig E.
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Ellison, Eric T.
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Menzel, Manuel D.
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Urai, Janos L.
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Hirth, Greg
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Rioux, Matthew
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Stockli, Daniel F.
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Lafay, Romain
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Beinlich, Andreas M.
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Coggon, Jude A.
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Warsi, Nehal H.
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Matter, Jürg M.
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Teagle, Damon A. H.
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Harris, Michelle
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Michibayashi, Katsuyoshi
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Takazawa, Eiichi
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Al Sulaimani, Zaher
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1 February 2022
Kelemen, Peter B.
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Carlos De Obeso, Juan
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Leong, James A.
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Godard, Marguerite
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Okazaki, Keishi
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Kotowski, Alissa J.
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Manning, Craig E.
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Ellison, Eric T.
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Menzel, Manuel D.
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Urai, Janos L.
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Hirth, Greg
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Rioux, Matthew
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Stockli, Daniel F.
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Lafay, Romain
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Beinlich, Andreas M.
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Coggon, Jude A.
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Warsi, Nehal H.
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Matter, Jürg M.
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Teagle, Damon A. H.
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Harris, Michelle
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Michibayashi, Katsuyoshi
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Takazawa, Eiichi
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Al Sulaimani, Zaher
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Kelemen, Peter B., Carlos De Obeso, Juan, Leong, James A., Godard, Marguerite, Okazaki, Keishi, Kotowski, Alissa J., Manning, Craig E., Ellison, Eric T., Menzel, Manuel D., Urai, Janos L., Hirth, Greg, Rioux, Matthew, Stockli, Daniel F., Lafay, Romain, Beinlich, Andreas M., Coggon, Jude A., Warsi, Nehal H., Matter, Jürg M., Teagle, Damon A. H., Harris, Michelle, Michibayashi, Katsuyoshi, Takazawa, Eiichi and Al Sulaimani, Zaher
(2022)
Listvenite formation during mass transfer into the leading edge of the mantle wedge: initial results from Oman Drilling Project Hole BT1B.
Journal of Geophysical Research: Solid Earth, 127 (2), [e2021JB022352].
(doi:10.1029/2021JB022352).
Abstract
This paper provides an overview of research on core from Oman Drilling Project Hole BT1B and the surrounding area, plus new data and calculations, constraining processes in the Tethyan subduction zone beneath the Samail ophiolite. The area is underlain by gently dipping, broadly folded layers of allochthonous Hawasina pelagic sediments, the metamorphic sole of the Samail ophiolite, and Banded Unit peridotites at the base of the Samail mantle section. Despite reactivation of some faults during uplift of the Jebel Akdar and Saih Hatat domes, the area preserves the tectonic “stratigraphy” of the Cretaceous subduction zone. Gently dipping listvenite bands, parallel to peridotite banding and to contacts between the peridotite and the metamorphic sole, replace peridotite at and near the basal thrust. Listvenites formed at less than 200°C and (poorly constrained) depths of 25–40 km by reaction with CO2-rich, aqueous fluids migrating from greater depths, derived from devolatilization of subducting sediments analogous to clastic sediments in the Hawasina Formation, at 400°–500°. Such processes could form important reservoirs for subducted CO2. Listvenite formation was accompanied by ductile deformation of serpentinites and listvenites—perhaps facilitated by fluid-rock reaction—in a process that could lead to aseismic subduction in some regions. Addition of H2O and CO2 to the mantle wedge, forming serpentinites and listvenites, caused large increases in the solid mass and volume of the rocks. This may have been accommodated by fractures formed as a result of volume changes, mainly at a serpentinization front.
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More information
Accepted/In Press date: 24 December 2021
e-pub ahead of print date: 13 January 2022
Published date: 1 February 2022
Additional Information:
Funding Information:
Drilling and research in the Oman Drilling Project were supported by the Alfred P. Sloan Foundation (in association with the Deep Carbon Observatory, DCO), the International Continental scientific Drilling Program (ICDP), US National Science Foundation (NSF) Research Grant NSF-EAR-1516300, the Japanese Marine Science and Technology Center (JAMSTEC), Grant No. 16H06347 from the Japanese Society for the Promotion of Science (JSPS), the US National Aeronautics and Space Administration (NASA, including the Rock Powered Life NASA Astrobiology Institute (NNA15BB02 A), the European Science Foundation, the German Science Foundation, the Swiss Science Foundation, and the International Ocean Discovery Program (aka International Ocean Drilling Program, IODP). Kelemen's research was also supported with funds from the Arthur D. Storke Chair at Columbia University. In addition to the authors of this paper, a huge team contributed to the success of OmanDP, including drilling and core analyses at Hole BT1B. In Oman, a Project Supervisory Committee chaired by Dr. Said Al Habsi (Director General of Water Resources Assessment in the Ministry of Regional Municipalities and Water Resources), and including Prof. Sobhi Nasir at Sultan Qaboos University, Dr. Ali Al Rajhi, Director of the Geological Survey of Oman, and others, ensured that the project went forward smoothly in accordance with Omani requirements. At Petroleum Development Oman (PDO), Dr. Hamad Shuaili and Dr. Hisham Siyabi kindly facilitated storage of the archive half of all OmanDP core. We particularly thank Dr. Jay Miller and Dr. Brad Clement at IODP TAMU for making the online proceedings volume possible, and Shana Lewis, Rhonda Kappler, Jean Wulfson, Phil Rumford, Lorri Peters, Crystal Wolfe and Kenneth Sherar at IODP TAMU for editorial assistance in preparing the Proceedings of the Oman Drilling Project, more or less following IODP protocols in presenting the results of this decidedly non-standard ICDP project. We thank the technical staff onboard Drilling Vessel Chikyu for fantastic, efficient support and advice over four months in summers 2017 and 2018, especially Lena Maeda, Dr. Yusuke Kubo, and Dr. Chiaki Igarashi. Dr. Nobu Eguchi served as a patient, generous liaison between OmanDP, NSF and JAMSTEC. Core description onboard Chikyu would have been impossible without proactive support from JAMSTEC President Asahiko Taira and NSF Program Director Leonard Johnson. Similarly, we received essential assistance with borehole permitting from Professor Ali Al Bemani, Vice Chancellor of Sultan Qaboos University. On a different timescale, we are deeply indebted to His Majesty Sultan Qaboos bin Said Al Said for his open-door policy for scientific research in Oman, and to Professors Françoise Boudier, Bob Coleman, Cliff Hopson and Adolphe Nicolas for establishing the framework for modern studies of the Samail ophiolite. Suggestions from Othmar Müntener, an anonymous reviewer, and Associate Editor John Lassiter led to substantial improvements of this paper.
Funding Information:
Drilling and research in the Oman Drilling Project were supported by the Alfred P. Sloan Foundation (in association with the Deep Carbon Observatory, DCO), the International Continental scientific Drilling Program (ICDP), US National Science Foundation (NSF) Research Grant NSF‐EAR‐1516300, the Japanese Marine Science and Technology Center (JAMSTEC), Grant No. 16H06347 from the Japanese Society for the Promotion of Science (JSPS), the US National Aeronautics and Space Administration (NASA, including the Rock Powered Life NASA Astrobiology Institute (NNA15BB02 A), the European Science Foundation, the German Science Foundation, the Swiss Science Foundation, and the International Ocean Discovery Program (aka International Ocean Drilling Program, IODP). Kelemen's research was also supported with funds from the Arthur D. Storke Chair at Columbia University. In addition to the authors of this paper, a huge team contributed to the success of OmanDP, including drilling and core analyses at Hole BT1B. In Oman, a Project Supervisory Committee chaired by Dr. Said Al Habsi (Director General of Water Resources Assessment in the Ministry of Regional Municipalities and Water Resources), and including Prof. Sobhi Nasir at Sultan Qaboos University, Dr. Ali Al Rajhi, Director of the Geological Survey of Oman, and others, ensured that the project went forward smoothly in accordance with Omani requirements. At Petroleum Development Oman (PDO), Dr. Hamad Shuaili and Dr. Hisham Siyabi kindly facilitated storage of the archive half of all OmanDP core. We particularly thank Dr. Jay Miller and Dr. Brad Clement at IODP TAMU for making the online proceedings volume possible, and Shana Lewis, Rhonda Kappler, Jean Wulfson, Phil Rumford, Lorri Peters, Crystal Wolfe and Kenneth Sherar at IODP TAMU for editorial assistance in preparing the Proceedings of the Oman Drilling Project, more or less following IODP protocols in presenting the results of this decidedly non‐standard ICDP project. We thank the technical staff onboard Drilling Vessel Chikyu for fantastic, efficient support and advice over four months in summers 2017 and 2018, especially Lena Maeda, Dr. Yusuke Kubo, and Dr. Chiaki Igarashi. Dr. Nobu Eguchi served as a patient, generous liaison between OmanDP, NSF and JAMSTEC. Core description onboard Chikyu would have been impossible without proactive support from JAMSTEC President Asahiko Taira and NSF Program Director Leonard Johnson. Similarly, we received essential assistance with borehole permitting from Professor Ali Al Bemani, Vice Chancellor of Sultan Qaboos University. On a different timescale, we are deeply indebted to His Majesty Sultan Qaboos bin Said Al Said for his open‐door policy for scientific research in Oman, and to Professors Françoise Boudier, Bob Coleman, Cliff Hopson and Adolphe Nicolas for establishing the framework for modern studies of the Samail ophiolite. Suggestions from Othmar Müntener, an anonymous reviewer, and Associate Editor John Lassiter led to substantial improvements of this paper.
Publisher Copyright:
© 2022. American Geophysical Union. All Rights Reserved.
Keywords:
Oman, Samail ophiolite, carbon cycle, ductile deformation, listvenite, subduction
Identifiers
Local EPrints ID: 472408
URI: http://eprints.soton.ac.uk/id/eprint/472408
ISSN: 2169-9313
PURE UUID: 755a16ce-1bf9-4ffc-b669-176e8a0a28b3
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Date deposited: 05 Dec 2022 17:36
Last modified: 17 Mar 2024 03:30
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Contributors
Author:
Peter B. Kelemen
Author:
Juan Carlos De Obeso
Author:
James A. Leong
Author:
Marguerite Godard
Author:
Keishi Okazaki
Author:
Alissa J. Kotowski
Author:
Craig E. Manning
Author:
Eric T. Ellison
Author:
Manuel D. Menzel
Author:
Janos L. Urai
Author:
Greg Hirth
Author:
Matthew Rioux
Author:
Daniel F. Stockli
Author:
Romain Lafay
Author:
Andreas M. Beinlich
Author:
Jude A. Coggon
Author:
Nehal H. Warsi
Author:
Michelle Harris
Author:
Katsuyoshi Michibayashi
Author:
Eiichi Takazawa
Author:
Zaher Al Sulaimani
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