U.S. Geological Survey Water - Supply Paper, 2255. Effect of eustatic sea-level changes on saltwater -freshwater in the northern atlantic coastal plain / Meisler, H.

Public ISBD Titre de série : U.S. Geological Survey Water - Supply Paper, 2255 Titre : Effect of eustatic sea-level changes on saltwater -freshwater in the northern atlantic coastal plain Type de document : texte imprimé Auteurs : Meisler, H. ; Leahy, P. P. ; Knobel, L. L. Mention d'édition : United States Government Printing Office Editeur : United States Government Printing Office Année de publication : 1984 ISBN/ISSN/EAN : CI-04174 Note générale : This paper explains the effect of eustatic sea-level changes on the physical and chimical relations between fresh and salty ground water in the northern Atlantic coastal plain and adjacent continental shels. It is part of a study by the U.S geological survey entitled regional aquifer system analysis of the northern atlantic coastal plain. Langues : Anglais (eng) Mots-clés : Hydrogéologie  Informatique  Modélisation  Simulation  Eau douce  Eau salée  Géochimie  Informatique appliquée  Etats Unis Index. décimale : 551 Géologie, météorologie, hydrologie générale Résumé : This paper explains the effect of eustatic sea-level changes on the physical and chimical relations between fresh and salty ground water in the northern Atlantic coastal plain and adjacent continental shels. It is part of a study by the U.S geological survey entitled regional aquifer system analysis of the northern atlantic coastal plain. Note de contenu : This paper explains the effect of eustatic sea-level changes on the physical and chimical relations between fresh and salty ground water in the northern Atlantic coastal plain and adjacent continental shels. It is part of a study by the U.S geological survey entitled regional aquifer system analysis of the northern atlantic coastal plain. U.S. Geological Survey Water - Supply Paper, 2255. Effect of eustatic sea-level changes on saltwater -freshwater in the northern atlantic coastal plain [texte imprimé] / Meisler, H. ; Leahy, P. P. ; Knobel, L. L.  . -  United States Government Printing Office . - United States Government Printing Office, 1984. ISSN : CI-04174 This paper explains the effect of eustatic sea-level changes on the physical and chimical relations between fresh and salty ground water in the northern Atlantic coastal plain and adjacent continental shels. It is part of a study by the U.S geological survey entitled regional aquifer system analysis of the northern atlantic coastal plain. Langues : Anglais (eng) Mots-clés : Hydrogéologie  Informatique  Modélisation  Simulation  Eau douce  Eau salée  Géochimie  Informatique appliquée  Etats Unis Index. décimale : 551 Géologie, météorologie, hydrologie générale Résumé : This paper explains the effect of eustatic sea-level changes on the physical and chimical relations between fresh and salty ground water in the northern Atlantic coastal plain and adjacent continental shels. It is part of a study by the U.S geological survey entitled regional aquifer system analysis of the northern atlantic coastal plain. Note de contenu : This paper explains the effect of eustatic sea-level changes on the physical and chimical relations between fresh and salty ground water in the northern Atlantic coastal plain and adjacent continental shels. It is part of a study by the U.S geological survey entitled regional aquifer system analysis of the northern atlantic coastal plain.

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U.S. Geological Survey Water Supply paper, 2323. Aqueous geochemistry of the Magothy aquifer, Maryland / Knobel, L. L.

Public ISBD Titre de série : U.S. Geological Survey Water Supply paper, 2323 Titre : Aqueous geochemistry of the Magothy aquifer, Maryland Type de document : texte imprimé Auteurs : Knobel, L. L. ; Phillips, S. W. Mention d'édition : United States Gouvernment Printing Office Editeur : United States Gouvernment Printing Office Année de publication : 1988 ISBN/ISSN/EAN : CI-05086 Note générale : The Upper Cretaceous Magothy formation of the Atlantic coastal plain is a seaward-dipping strand-zone deposit of fluviomarine origin that crops out in irregular belt in Maryland. Southwest of the outcrop, the Magothy formation is overlain by younger strata. Chemical analyses of water samples from the Magothy aquifer, Maryland, indicate several hydrochemical facies. The origin of these hydrochemical facies is related to the source of recharge an the chemical processes that occur as water flows downgradient. Langues : Anglais (eng) Mots-clés : Eau souterraine  Hydrochimie  Bassin HYDROGEOLOGIE  Hydrogéologie  Géochimie aqueuse  Bassin versant de Magothy  Stabilité minérale  Evolution chimique Index. décimale : 551.48 Hydrologie : Résumé : The Upper Cretaceous Magothy formation of the Atlantic coastal plain is a seaward-dipping strand-zone deposit of fluviomarine origin that crops out in irregular belt in Maryland. Southwest of the outcrop, the Magothy formation is overlain by younger strata. Chemical analyses of water samples from the Magothy aquifer, Maryland, indicate several hydrochemical facies. The origin of these hydrochemical facies is related to the source of recharge an the chemical processes that occur as water flows downgradient. Note de contenu : The Upper Cretaceous Magothy formation of the Atlantic coastal plain is a seaward-dipping strand-zone deposit of fluviomarine origin that crops out in irregular belt in Maryland. Southwest of the outcrop, the Magothy formation is overlain by younger strata. Chemical analyses of water samples from the Magothy aquifer, Maryland, indicate several hydrochemical facies. The origin of these hydrochemical facies is related to the source of recharge an the chemical processes that occur as water flows downgradient. U.S. Geological Survey Water Supply paper, 2323. Aqueous geochemistry of the Magothy aquifer, Maryland [texte imprimé] / Knobel, L. L. ; Phillips, S. W.  . -  United States Gouvernment Printing Office . - United States Gouvernment Printing Office, 1988. ISSN : CI-05086 The Upper Cretaceous Magothy formation of the Atlantic coastal plain is a seaward-dipping strand-zone deposit of fluviomarine origin that crops out in irregular belt in Maryland. Southwest of the outcrop, the Magothy formation is overlain by younger strata. Chemical analyses of water samples from the Magothy aquifer, Maryland, indicate several hydrochemical facies. The origin of these hydrochemical facies is related to the source of recharge an the chemical processes that occur as water flows downgradient. Langues : Anglais (eng) Mots-clés : Eau souterraine  Hydrochimie  Bassin HYDROGEOLOGIE  Hydrogéologie  Géochimie aqueuse  Bassin versant de Magothy  Stabilité minérale  Evolution chimique Index. décimale : 551.48 Hydrologie : Résumé : The Upper Cretaceous Magothy formation of the Atlantic coastal plain is a seaward-dipping strand-zone deposit of fluviomarine origin that crops out in irregular belt in Maryland. Southwest of the outcrop, the Magothy formation is overlain by younger strata. Chemical analyses of water samples from the Magothy aquifer, Maryland, indicate several hydrochemical facies. The origin of these hydrochemical facies is related to the source of recharge an the chemical processes that occur as water flows downgradient. Note de contenu : The Upper Cretaceous Magothy formation of the Atlantic coastal plain is a seaward-dipping strand-zone deposit of fluviomarine origin that crops out in irregular belt in Maryland. Southwest of the outcrop, the Magothy formation is overlain by younger strata. Chemical analyses of water samples from the Magothy aquifer, Maryland, indicate several hydrochemical facies. The origin of these hydrochemical facies is related to the source of recharge an the chemical processes that occur as water flows downgradient.

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