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.

Réservation

Réserver ce document

Exemplaires(8)

Code-barres	Cote	Support	Localisation	Section	Disponibilité
CI03B086.62664	CI-05086	Monographie	Bibliothèque CDI-Ouaga	Fond documentaire	Disponible
CI03B086.62663	CI-05086	Monographie	Bibliothèque CDI-Ouaga	Fond documentaire	Disponible
CI03B086.62662	CI-05086	Monographie	Bibliothèque CDI-Ouaga	Fond documentaire	Disponible
CI03B086.62661	CI-05086	Monographie	Bibliothèque CDI-Ouaga	Fond documentaire	Disponible
CI03B086.62660	CI-05086	Monographie	Bibliothèque CDI-Ouaga	Fond documentaire	Disponible
CI03B086.62659	CI-05086	Monographie	Bibliothèque CDI-Ouaga	Fond documentaire	Disponible
CI03B086.62658	CI-05086	Monographie	Bibliothèque CDI-Ouaga	Fond documentaire	Disponible
CI03B086.62657	CI-05086	Monographie	Bibliothèque CDI-Ouaga	Fond documentaire	Disponible

---

1 (1 - 1 / 1) Par page : 25 50 100 200