Provenance of Nicobar Fan sediments from IODP Expedition 362, offshore Sumatra (NERC grant NE/P016618/1)
Detrital zircon age data, details of Expedition 362 samples . For more information see published report, https://doi.org/10.1016/j.epsl.2017.07.019 IODP Sites U1480–U1481, located on the Indian oceanic plate, east of the NinetyEast Ridge and west of the north Sumatran subduction margin Site U1480 ~ 3°2.0447'N 91°36.3481'E 4147.5 Site U1481 ~ 2°45.261'N 91°45.5771'E
dataset
https://doi.org/10.1016/j.epsl.2017.07.019
function: information
http://www.bgs.ac.uk/services/ngdc/accessions/index.html#item112129
function: download
http://data.bgs.ac.uk/id/dataHolding/13607363
eng
geoscientificInformation
publication
2008-06-01
Provenance
Submarine fans
Zircon
NGDC Deposited Data
Radiometric dating
revision
2022
NERC_DDC
91.6000
91.7700
3.0300
2.7500
revision
2010
INDIAN OCEAN [id=2001427]
2016-08-06
2016-10-06
creation
2018-08-08
notApplicable
Detrital zircon age analysis for provenance of Nicobar Fan sands Samples were taken from sediment gravity flow deposits in cores of Sites U1480 and U1481. A concentrate of heavy minerals rich in zircon obtained using standard heavy liquid techniques was mounted in araldite and polished. Zircon grains were selected randomly and analysed by laser ablation inductively coupled plasma mass spectrometry in the London Geochronology Centre at University College London using a New Wave 193 nm aperture-imaged, frequency-quintupled laser ablation system coupled to an Agilent 7700 ICPMS. Typical ablation parameters were 20-35 µm, 10 Hz repetition rate and an energy fluence of ca. 2:5 J/cm2. Plesovice was used as an age standard (TIMS reference age 337.13±0.37 Ma) to correct for instrumental mass bias and depth-dependent inter-element fractionation of Pb, Th and U. Temora and 91500 zircon were used as secondary age standards. Data were processed using GLITTER 4.4 data reduction software. Calculated 206Pb/238U ages were used for grains younger than 1000 Ma, and the 207Pb/206Pb age for older grains. Grains with a complex growth history or disturbed isotopic ratios, with > +5/-15% discordance, were rejected.
publication
2011
false
See the referenced specification
publication
2010-12-08
false
See http://eur-lex.europa.eu/LexUriServ/LexUriServ.do?uri=OJ:L:2010:323:0011:0102:EN:PDF
MS Excel
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Department of Earth Sciences
University College London
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British Geological Survey
Environmental Science Centre,Keyworth
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United Kingdom
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pointOfContact
2025-03-24