Difference between revisions of "Meteoric diagenesis"
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− | Meteoric diagenesis is the modification of deposits at or near the surface in the [[phreatic]] and [[vadose]] zones.<ref name=Scholle> Scholle,P.A., and D. Ulmer-Scholle, 2003, A color guide to the petrography of carbonate rocks: Grains, textures, porosity, diagenesis: [http://store.aapg.org/detail.aspx?id=649 AAPG Memoir 77] p. 332-350</ref> | + | Meteoric diagenesis is the modification of deposits at or near the surface in the [[phreatic]] and [[vadose]] zones.<ref name=Scholle> Scholle, P. A., and D. Ulmer-Scholle, 2003, [http://archives.datapages.com/data/specpubs/memoir77/m77ch24/m77ch24.htm Eogenetic Meteoric Diagenesis] in Scholle, P. A. & D. Ulmer-Scholle, eds, A color guide to the petrography of carbonate rocks: Grains, textures, porosity, diagenesis: [http://store.aapg.org/detail.aspx?id=649 AAPG Memoir 77] p. 332-350</ref> |
==References== | ==References== | ||
{{Reflist}} | {{Reflist}} | ||
{{stub}} | {{stub}} |
Revision as of 21:04, 13 March 2014
Meteoric diagenesis is the modification of deposits at or near the surface in the phreatic and vadose zones.[1]
References
- ↑ Scholle, P. A., and D. Ulmer-Scholle, 2003, Eogenetic Meteoric Diagenesis in Scholle, P. A. & D. Ulmer-Scholle, eds, A color guide to the petrography of carbonate rocks: Grains, textures, porosity, diagenesis: AAPG Memoir 77 p. 332-350
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