Oxygen and strontium isotopes and Rb and Ba were determined in interstitial water (IW) collected from Sites 1109, 1115, and 1118 drilled on the Woodlark Rise during Ocean Drilling Program Leg 180. The trace element and mineralogical composition of the clay fraction of sediments isolated from the squeeze cakes corresponding to IW samples from Site 1109 was also determined.
1De Carlo, E.H., Lackschewitz, K.K., and Carmody, R., 2001. Data report: Trace element and isotopic composition of interstitial water and sediments from the Woodlark Rise, ODP Leg 180. In Huchon, P., Taylor, B., and Klaus, A. (Eds.), Proc. ODP, Sci. Results, 180 [Online]. Available from World Wide Web: <http://www-odp.tamu.edu/publications/180_SR/160/160.htm>. [Cited YYYY-MM-DD]
2Department of Oceanography, SOEST, University of Hawaii at Manoa, Honolulu HI 96822, USA. edecarlo@soest.hawaii.edu
3Fachgebiet Petrologie der Ozeankruste, Fachbereich 5, Geowissenschaften Postfach 330 440, 28334 Bremen, Federal Republic of Germany.
4SOEST, University of Hawaii at Manoa, Honolulu HI 96822, USA.
Initial
receipt: 14 December 2000
Acceptance: 7 July 2001
Web publication: 2 November 2001
Ms 180SR-160