Downloads provided by UsageCountsIODP Expedition 366 ICP-AES elemental analysis (interstitial water)
Fryer, P.; Wheat, C.G.; Williams, T.; Albers, E.; Bekins, B.; Debret, B.P.R.; Deng, J.; Dong, Y.; Eickenbusch, P.; Frery, E.A.; Ichiyama, Y.; Johnson, K.; Johnston, R.M.; Kevorkian, R.T.; Kurz, W.; Magalhaes, V.; Mantovanelli, S.S.; Menapace, W.; Menzies, C.D.; Michibayashi, K.; Moyer, C.L.; Mullane, K.K.; Park, J.-W.; Price, R.E.; Ryan, J.G.; Shervais, J.W.; Sissmann, O.J.; Suzuki, S.; Takai, K.; Walter, B.; Zhang, R.;
IODP Expedition 366 ICP-AES elemental analysis (interstitial water)
Elemental concentration in interstitial water samples was measured by inductively coupled plasma - atomic emission spectroscopy (ICP-AES). Data are presented by element-wavelength pair (e.g., more than one calcium line may be reported). Elemental lines for which data do not exist for a particular expedition will not appear.
seismic zones, forearc, Pacific plate, Expedition 366, Conical Seamount, Leg 195, Earth in Motion, JOIDES Resolution, Asut Tesoru Seamount, Celestial Seamount, serpentinite, Site 1200, Ynazao Seamount, mud volcano, guyot, subseafloor biosphere, CORK, Big Blue Seamount, Fantangisna Seamount, Mariana, Blue Moon Seamount, ultramafic rock, Deep biosphere, harzburgite, South Chamorro Seamount, Site U1493, Site U1494, Site U1491, Site U1492, Site U1497, Site U1498, subduction, reef limestone, Site U1495, Site U1496, seismogenic zone
seismic zones, forearc, Pacific plate, Expedition 366, Conical Seamount, Leg 195, Earth in Motion, JOIDES Resolution, Asut Tesoru Seamount, Celestial Seamount, serpentinite, Site 1200, Ynazao Seamount, mud volcano, guyot, subseafloor biosphere, CORK, Big Blue Seamount, Fantangisna Seamount, Mariana, Blue Moon Seamount, ultramafic rock, Deep biosphere, harzburgite, South Chamorro Seamount, Site U1493, Site U1494, Site U1491, Site U1492, Site U1497, Site U1498, subduction, reef limestone, Site U1495, Site U1496, seismogenic zone
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This indicator reflects the initial momentum of an article directly after its publication, based on the underlying citation network.
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