Geochemical evolution of a sublacustrine hydrothermal vent system: Temporal constraints imposed by reactive transport modeling
- 8 June 2022
- journal article
- research article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 331, 18-34
Abstract
No abstract availableKeywords
Funding Information
- China Scholarship Council (201904910227)
- National Science Foundation (EAR-1515377)
- National Natural Science Foundation of China (41702273)
This publication has 64 references indexed in Scilit:
- Numerical simulation of magmatic hydrothermal systemsReviews of Geophysics, 2010
- Monitoring a Supervolcano in Repose: Heat and Volatile Flux at the Yellowstone CalderaElements, 2008
- Hydrothermal and tectonic activity in northern Yellowstone Lake, WyomingGeological Society of America Bulletin, 2003
- Exploration and discovery in Yellowstone Lake: results from high-resolution sonar imaging, seismic reflection profiling, and submersible studiesJournal of Volcanology and Geothermal Research, 2003
- On fluid flow and mineral alteration in fractured caprock of magmatic hydrothermal systemsJournal of Geophysical Research, 2001
- The effect of malonate on the dissolution kinetics of albite, quartz, and microcline as a function of pH at 70°CApplied Geochemistry, 1995
- A coupled model for transport of multiple chemical species and kinetic precipitation/dissolution reactions with application to reactive flow in single phase hydrothermal systemsAmerican Journal of Science, 1994
- Relative Solubility of Corundum, Gibbsite, Boehmite, and Diaspore at Standard State ConditionsClays and Clay Minerals, 1988
- A problem posed by vapour-dominated geothermal systemsNature, 1980
- Intrusion of basaltic sills into highly porous sediments, and resulting hydrothermal activityNature, 1980