Hydrochemical processes in the lower Jordan valley and in the Dead Sea area

Keyphrases

• Dead Sea 100%
• Jordan Valley 100%
• Dead Sea Area 100%
• Hydrochemical 100%
• Groundwater 85%
• Brine 71%
• SO42- 57%
• Judea 42%
• Freshwater 28%
• Leaching 28%
• Dolomite 28%
• Recharge Area 28%
• Gd Anomaly 28%
• Drainage Basin 14%
• Highlands 14%
• Distribution Pattern 14%
• Saline Water 14%
• Molar Ratio 14%
• Seawater 14%
• Trace Elements 14%
• Jordan 14%
• Sulfide 14%
• Jordan River 14%
• Magnetic Anomaly 14%
• Gypsum 14%
• Deep-seated 14%
• Ion Exchange 14%
• Rare Earth 14%
• Clay Minerals 14%
• Endmember 14%
• Sedimentary Rocks 14%
• Produced Water 14%
• Geological Origin 14%
• Spiders 14%
• Groundwater Samples 14%
• Chemical Features 14%
• Lisan Formation 14%
• Lisan 14%
• Upper Cretaceous 14%
• Lower Cretaceous 14%
• Lake Lisan 14%
• Sedom 14%
• Anhydrite 14%
• Bearing Body 14%
• Volcanic 14%
• Lower Jordan River 14%
• B Content 14%
• Lake Tiberias 14%
• Hot Brine 14%
• Saline Groundwater 14%
• Salinity Increase 14%
• Groundwater Circulation 14%
• Discharge Water 14%
• Marine Sulfate 14%
• Hot Saline 14%
• Anthropogenic Gd 14%
• Regional Aquifer 14%
• Plagioclase 14%
• Albitization 14%
• Deep Groundwater 14%
• Rift Faults 14%
• Major Element Composition 14%
• Epsomite 14%

Earth and Planetary Sciences

• Jordan 100%
• Dolomite 66%
• Salinity 66%
• Jordan River 66%
• Drainage Basin 33%
• Trace Element 33%
• Sea Level 33%
• Calcite 33%
• Sedimentary Rock 33%
• Lower Cretaceous 33%
• Anhydrite 33%
• Upper Cretaceous 33%
• Groundwater Circulation 33%
• Albitization 33%
• Mineral Control 33%
• Magnetic Anomalies 33%
• Ion Exchange 33%
• Clay Mineral 33%