ON THE ORIGIN OF FLUIDS INCLUDED IN PHANEROZOIC MARINE HALITE-BASIC INTERPRETATION STRATEGIES

dc.contributor.author	Zimmermann H.
dc.date.accessioned	2021-02-09T10:08:09Z
dc.date.available	2021-02-09T10:08:09Z
dc.date.issued	2001
dc.identifier	https://www.elibrary.ru/item.asp?id=542478
dc.identifier.citation	Geochimica et Cosmochimica Acta, 2001, 65, 1, 35-45
dc.identifier.issn	0016-7037
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/24557
dc.description.abstract	In addition to the use of Janecke units in the NaCl-KCl-MgCl2-Na2SO4-H2O/NaCl-KCl-MgCl2-CaCl2-H2O system to classify brine origins, a fast and efficient method is described to identify inclusions of evaporated seawater in (ancient) marine halite. The method is based on the calculation of degrees of evaporation for various elements (DEELEMENT) of brines created by different salt forming processes. The DEELEMENT patterns of the fluid inclusions serve as fingerprints and are characteristic of different brine types of known origin.
dc.title	ON THE ORIGIN OF FLUIDS INCLUDED IN PHANEROZOIC MARINE HALITE-BASIC INTERPRETATION STRATEGIES
dc.type	Статья

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