How to cite this dataset:
Ryb, U., Erel, Y., Matthews, A., Avni, Y., Stern, D., 2022. Tables S1-8: Sr, Pb, O, C, Mo and Fe isotope data measured in epigenetic dolomite and ferric oxide minerals from the Negev Desert, southern Israel., Version 1.0. Interdisciplinary Earth Data Alliance (IEDA).
https://doi.org/10.26022/IEDA/112700. Accessed 2024-07-26.
Related
Publication(s):
Erel, Y., Listovsky, N., Matthews, A., Ilani, S., and Avni, Y., 2006, Tracing end-member fluid sources in sub-surface iron mineralization and dolomitization along a proximal fault to the dead sea transform: Geochimica et Cosmochimica Acta, v. 70, p. 5552–5570.
Grosz, S., Matthews, A., Ilani, S., Ayalon, A., and Garfunkel, Z., 2006, Iron mineralization and dolomitization in the Paran Fault zone, Israel: implications for low-temperature basinal fluid processes near the Dead Sea Transform: Geofluids, v. 6, p. 137–153.
Stein, M., Agnon, A., Katz, A., and Starinsky, A., 2002, Strontium isotopes in discordant dolomite bodies of the Judea Group, Dead Sea basin: Israel Journal of Earth Sciences, v. 51, p. 219–224.
Ryb, U., Erel, Y., Matthews, A., Avni, Y., Gordon, G.W., and Anbar, A.D., 2009, Large molybdenum isotope variations trace subsurface fluid migration along the Dead Sea transform: Geology, v. 37, p. 463–466.
User Contributed Keyword(s):
Epigenetic mineralization, Divergent plate boundary, dolomite, ferric oxide, U-Pb dating