Abstract
Sites 812 through 814 and 824 reflect a zoned system with 87Sr/86Sr ratios close to modern seawater values despite the Miocene age of the host sediment. It is possible that the fluid flow at depth is associated with a hardground between Pliocene/Pleistocene and Miocene/Pliocene sediments. Pore waters from Sites 815, 817, 818 and 823 show increasing salinites/chloride with depth which may reflect the presence of evaporites beneath the drilled sections. -from Authors
| Original language | English (US) |
|---|---|
| Pages (from-to) | 473-480 |
| Number of pages | 8 |
| Journal | Unknown Journal |
| DOIs | |
| State | Published - Jan 1 1993 |
| Externally published | Yes |
ASJC Scopus subject areas
- Environmental Science(all)
- Earth and Planetary Sciences(all)
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Elderfield, H., Swart, P. K., McKenzie, J. A., & Williams, A. (1993). The strontium isotopic composition of pore waters from Leg 133: northeast Australian margin. Unknown Journal, 473-480. https://doi.org/10.2973/odp.proc.sr.133.253.1993