Boron and chlorine contents of upper oceanic crust: basement samples from IODP Hole 1256D
Boron and chlorine contents of upper oceanic crust: basement samples from IODP Hole 1256D
Boron, Cl, Ti, K, Sm, and Gd concentrations of oceanic crust samples were determined by prompt gamma neutron activation analysis. The samples include 63 basalts and 5 gabbros obtained at various depths (369–1503 m below seafloor) from Hole 1256D during Ocean Drilling Program Leg 206 and Integrated Ocean Drilling Program Expedition 309 and 312. The results show stepwise downhole variations, B content and B/K decrease, and Cl content and Cl/K increase with increasing depth. High B content (>1.5 ppm) in shallower rocks (extrusive lavas) is probably achieved by low-temperature seawater alteration, and high Cl contents (up to 1400 ppm) in the deeper rocks (plutonic section) would show result of high-temperature hydrothermal alteration. Average B and Cl values for the upper oceanic crust in Hole 1256D are 1.5 ppm and 334 ppm, respectively.
Q12O15
Sano, Takashi
9175ab5f-a44f-462a-8a57-b43fe3807308
Miyoshi, Masaya
02a9e0c3-99fa-4665-ad39-9a2264e5d756
Ingle, Stephanie
290ddc48-9f8a-4639-86a7-d552434de4e8
Banerjee, Neil R.
5d39afaa-a973-40f5-9aa1-91d68e50745a
Ishimoto, Mitsunori
19fbae88-2c6d-4ace-b2fa-554a551f883c
Fukuoka, Takaaki
9f466e25-9616-4fb7-b9c6-524f7caf1679
5 December 2008
Sano, Takashi
9175ab5f-a44f-462a-8a57-b43fe3807308
Miyoshi, Masaya
02a9e0c3-99fa-4665-ad39-9a2264e5d756
Ingle, Stephanie
290ddc48-9f8a-4639-86a7-d552434de4e8
Banerjee, Neil R.
5d39afaa-a973-40f5-9aa1-91d68e50745a
Ishimoto, Mitsunori
19fbae88-2c6d-4ace-b2fa-554a551f883c
Fukuoka, Takaaki
9f466e25-9616-4fb7-b9c6-524f7caf1679
Sano, Takashi, Miyoshi, Masaya, Ingle, Stephanie, Banerjee, Neil R., Ishimoto, Mitsunori and Fukuoka, Takaaki
(2008)
Boron and chlorine contents of upper oceanic crust: basement samples from IODP Hole 1256D.
Geochemistry, Geophysics, Geosystems, 9, .
(doi:10.1029/2008GC002182).
Abstract
Boron, Cl, Ti, K, Sm, and Gd concentrations of oceanic crust samples were determined by prompt gamma neutron activation analysis. The samples include 63 basalts and 5 gabbros obtained at various depths (369–1503 m below seafloor) from Hole 1256D during Ocean Drilling Program Leg 206 and Integrated Ocean Drilling Program Expedition 309 and 312. The results show stepwise downhole variations, B content and B/K decrease, and Cl content and Cl/K increase with increasing depth. High B content (>1.5 ppm) in shallower rocks (extrusive lavas) is probably achieved by low-temperature seawater alteration, and high Cl contents (up to 1400 ppm) in the deeper rocks (plutonic section) would show result of high-temperature hydrothermal alteration. Average B and Cl values for the upper oceanic crust in Hole 1256D are 1.5 ppm and 334 ppm, respectively.
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Published date: 5 December 2008
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Local EPrints ID: 65027
URI: http://eprints.soton.ac.uk/id/eprint/65027
ISSN: 1525-2027
PURE UUID: 209ced8f-786e-471e-bdc5-fe6c08bbfcd5
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Date deposited: 27 Jan 2009
Last modified: 15 Mar 2024 12:05
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Author:
Takashi Sano
Author:
Masaya Miyoshi
Author:
Stephanie Ingle
Author:
Neil R. Banerjee
Author:
Mitsunori Ishimoto
Author:
Takaaki Fukuoka
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