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Hanaa Deik

Geowissenschaftlerin

Name	Hanaa Deik
Ort	Latakia Deutschland Syrien
Akademischer Grad bzw. Titel	Dr. rer. nat., M.Sc.
Beruf	Geowissenschaftlerin (charakteristischer Beruf)
Variante	H. Deik
Quelle	Dissertation
Datensatztyp	Person
GND-Nummer	1211978303
Datensatz-ID	1211978303
Beteiligt an alle anzeigen Contrasting intensity of aragonite dissolution and dolomite cementation in glacial versus interglacial intervals of a subtropical carbonate succession Contrasting intensity of aragonite dissolution and dolomitecementation in glacial versus interglacial intervals of asubtropical carbonate succession Pliocene to Recent development of carbonate systems from the central and southern Indian Ocean (Maldives and West Australian Shelf) : primary cycles versus diagenetic influence The sedimentary record of Quaternary glacial to interglacial sea‐level change on a subtropical carbonate ramp : Southwest Shelf of Australia The sedimentary record of Quaternary glacial to interglacial sea‐level change on a subtropical carbonate ramp: Southwest Shelf of Australia Glacial Indonesian Throughflow weakening across the Mid-Pleistocene Climatic Transition Hardened faecal pellets as a significant component in deep water, subtropical marine environments

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Hanaa Deik

Contrasting intensity of aragonite dissolution and dolomite cementation in glacial versus interglacial intervals of a subtropical carbonate succession

Contrasting intensity of aragonite dissolution and dolomitecementation in glacial versus interglacial intervals of asubtropical carbonate succession

Pliocene to Recent development of carbonate systems from the central and southern Indian Ocean (Maldives and West Australian Shelf) : primary cycles versus diagenetic influence

The sedimentary record of Quaternary glacial to interglacial sea‐level change on a subtropical carbonate ramp : Southwest Shelf of Australia

The sedimentary record of Quaternary glacial to interglacial sea‐level change on a subtropical carbonate ramp: Southwest Shelf of Australia

Glacial Indonesian Throughflow weakening across the Mid-Pleistocene Climatic Transition

Hardened faecal pellets as a significant component in deep water, subtropical marine environments