International Ocean Discovery Program
McNeill, L.C.
Dugan, B.
Petronotis, K.E.
Backman, J.
Bourlange, S.
Chemale, F.
Chen, W.
Colson, T.A.
Frederik, M.C.G.
Guèrin, G.
Hamahashi, M.
Henstock, T.
House, B.M.
Hüpers, A.
Jeppson, T.N.
Kachovich, S.
Kenigsberg, A.R.
Kuranaga, M.
Kutterolf, S.
Milliken, K.L.
Mitchison, F.L.
Mukoyoshi, H.
Nair, N.
Owari, S.
Pickering, K.T.
Pouderoux, H.F.A.
Shan, Y.
Song, I.
Torres, M.E.
Vannucchi, P.
Vrolijk, P.J.
Yang, T.
Zhao, X.
2020-03-31
<p>Inorganic carbon (carbonate) is determined by coulometry, which uses a photodetection cell to measure carbon dioxide evolved during sample acidification. Report includes percent inorganic carbon and calcium carbonate.</p>
https://doi.org/10.5281/zenodo.3752071
oai:zenodo.org:3752071
Zenodo
https://doi.org/10.14379/iodp.proc.362.2017
https://zenodo.org/communities/iodp
https://doi.org/10.5281/zenodo.3752070
info:eu-repo/semantics/openAccess
Creative Commons Zero v1.0 Universal
https://creativecommons.org/publicdomain/zero/1.0/legalcode
Expedition 362
Sumatra subduction zone
Site U1480
Site U1481
Earthquakes
Tsunami
JOIDES Resolution
Indian Ocean
Nicobar Fan
Ninetyeast Ridge
Sunda subduction zone
Andaman-Nicobar Islands
Wharton Basin
Indo-Australian plate
Bengal Fan
Himalaya
Sumatra-Andaman 2004 earthquake
shallow seismogenic slip
décollement
megathrust
forearc
IODP Expedition 362 Inorganic carbon (coulometer)
info:eu-repo/semantics/other