Article ID Journal Published Year Pages File Type
4706161 Geochimica et Cosmochimica Acta 2007 10 Pages PDF
Abstract
Pore fluids in compacting sedimentary basins of quartz sandstone are nearly saturated throughout most of diagenetic processes. Ultrafines and unstable surfaces produced by stress appear not to be the major sources of quartz cement.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
Preview
Evolution of fluid chemistry in quartz compaction systems: Experimental investigations and numerical modeling
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