Modern Iron Ooids of Hydrothermal Origin as a Proxy for Ancient Deposits-Reference-Cited by-同舟云学术

Modern Iron Ooids of Hydrothermal Origin as a Proxy for Ancient Deposits

Published:2019-05-08 Issue:1 Volume:9 Page:
ISSN:2045-2322
Container-title:Scientific Reports
language:en
Short-container-title:Sci Rep

Author:

Di Bella Marcella,Sabatino Giuseppe,Quartieri Simona,Ferretti Annalisa^ORCID,Cavalazzi Barbara,Barbieri Roberto,Foucher Frédéric^ORCID,Messori Fabio,Italiano Francesco^ORCID

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Link

http://www.nature.com/articles/s41598-019-43181-y.pdf

Reference50 articles.

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2. Brett, C. E., McLaughlin, P. I., Histon, K., Schindler, E. & Ferretti, A. Time-specific aspects of facies: State of the art, examples, and possible causes. Palaeogeogr. Palaeoclimatol. Palaeoecol. 367–368, 6–18 (2012).

3. Kimberley, M. M. Debate about ironstone: has solute supply been surficial weathering, hydrothermal convection, or exhalation of deep fluids? Terra Nova 6, 116–132 (1994).

4. Heikoop, J. M., Tsujita, C. J., Risk, M. J., Tomascik, T. & Mah, A. J. Modern iron ooids from a shallow-marine volcanic setting: Mahengetang, Indonesia. Geology 24, 759–762 (1996).

5. Sturesson, U., Dronov, A. & Saadre, T. Lower Ordovician iron ooids and associated oolitic clays in Russia and Estonia. Sediment. Geol. 123, 63–80 (1999).

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