[EAN: 9783639277760], Neubuch, [PU: VDM Verlag Dr. Müller], nach der Bestellung gedruckt Neuware - Printed after ordering - The Red Sea, one of the warmest and saltiest water bodies in th… Mehr…
[EAN: 9783639277760], Neubuch, [PU: VDM Verlag Dr. Müller], nach der Bestellung gedruckt Neuware - Printed after ordering - The Red Sea, one of the warmest and saltiest water bodies in the world, is a recent example for ocean basin formation by break of a continent, which makes it a perfect study area to investigate the early stage of the formation of an ocean basin (e.g. magma intrusion). This book provides new data of the two sediment cores from the Shaban Deep in the northern Red Sea. Although the two cores are located about a kilometer distance, distinctly different isotopic and geochemical signals were observed. Compared to the usual stable oxygen isotope ( 18O) signatures of planktonic foraminifera in the Red Sea, a strong negative 18O shift was seen in the core 17008-1. The planktonic foraminifera shells below 183 cm core depth, showed high degrees of diagenetic alteration. This alteration has not been caused by a hydrothermal input, but rather dominated by post-depositional alteration through hot pore-waters. The heat source is most likely to be basaltic intrusion occurred before 6 ka, and located close to the core 17008-1. These results will shed light on the geological construction of the Red Sea area as well as for investigating the hydrothermal activity and ore formation in the region. 92 pp. Englisch, Books<
The Red Sea, one of the warmest and saltiest water bodies in the world, is a recent example for ocean basin formation by break of a continent, which makes it a perfect study area to inves… Mehr…
The Red Sea, one of the warmest and saltiest water bodies in the world, is a recent example for ocean basin formation by break of a continent, which makes it a perfect study area to investigate the early stage of the formation of an ocean basin (e.g. magma intrusion). This book provides new data of the two sediment cores from the Shaban Deep in the northern Red Sea. Although the two cores are located about a kilometer distance, distinctly different isotopic and geochemical signals were observed. Compared to the usual stable oxygen isotope (δ18O) signatures of planktonic foraminifera in the Red Sea, a strong negative δ18O shift was seen in the core 17008-1. The planktonic foraminifera shells below 183 cm core depth, showed high degrees of diagenetic alteration. This alteration has not been caused by a hydrothermal input, but rather dominated by post-depositional alteration through hot pore-waters. The heat source is most likely to be basaltic intrusion occurred before 6 ka, and located close to the core 17008-1. These results will shed light on the geological construction of the Red Sea area as well as for investigating the hydrothermal activity and ore formation in the region. Trade Books>Trade Paperback>Nature & Wildlife>Geology & Weather>Geology & Weather, KS OmniScriptum Publishing Core >1<
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[EAN: 9783639277760], Neubuch, [PU: VDM Verlag Dr. Müller], This item is printed on demand - it takes 3-4 days longer - Neuware -The Red Sea, one of the warmest and saltiest water bodies … Mehr…
[EAN: 9783639277760], Neubuch, [PU: VDM Verlag Dr. Müller], This item is printed on demand - it takes 3-4 days longer - Neuware -The Red Sea, one of the warmest and saltiest water bodies in the world, is a recent example for ocean basin formation by break of a continent, which makes it a perfect study area to investigate the early stage of the formation of an ocean basin (e.g. magma intrusion). This book provides new data of the two sediment cores from the Shaban Deep in the northern Red Sea. Although the two cores are located about a kilometer distance, distinctly different isotopic and geochemical signals were observed. Compared to the usual stable oxygen isotope ( 18O) signatures of planktonic foraminifera in the Red Sea, a strong negative 18O shift was seen in the core 17008-1. The planktonic foraminifera shells below 183 cm core depth, showed high degrees of diagenetic alteration. This alteration has not been caused by a hydrothermal input, but rather dominated by post-depositional alteration through hot pore-waters. The heat source is most likely to be basaltic intrusion occurred before 6 ka, and located close to the core 17008-1. These results will shed light on the geological construction of the Red Sea area as well as for investigating the hydrothermal activity and ore formation in the region. 92 pp. Englisch, Books<
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BuchWeltWeit Inh. Ludwig Meier e.K., Bergisch Gladbach, Germany [57449362] [Rating: 5 (von 5)] NEW BOOK. Versandkosten:Versandkostenfrei. (EUR 0.00) Details...
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[EAN: 9783639277760], Neubuch, [PU: VDM Verlag Dr. M?ller], GEOWISSENSCHAFTEN GEOLOGIE CARBONATES \\"RED-SEA\\" SAHABAN DEEP PLANKTONIC FORAMINIFERA STABLE OXYGEN ISOTOPES CARBON DIAGENESIS ALTERATION RE-MINERALIZATION SEMIOT, Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Autor/Autorin: Olgun NazliPhD student in IFM-GEOMAR (Germany). She did her bachelors in Geological Engineering in the Middle East Technical University (Turkey) and masters in University of Kiel (Germany). Her research interests cover a wide range o., Books<
[ED: Kartoniert / Broschiert], [PU: VDM Verlag Dr. Mueller], Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Autor/Autorin: Olgun NazliPhD… Mehr…
[ED: Kartoniert / Broschiert], [PU: VDM Verlag Dr. Mueller], Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Autor/Autorin: Olgun NazliPhD student in IFM-GEOMAR (Germany). She did her bachelors in Geological Engineering in the Middle East Technical University (Turkey), DE, [SC: 0.00], Neuware, gewerbliches Angebot, Hardcover, 92, [GW: 155g], 1. Auflage, Banküberweisung, PayPal<
[EAN: 9783639277760], Neubuch, [PU: VDM Verlag Dr. Müller], nach der Bestellung gedruckt Neuware - Printed after ordering - The Red Sea, one of the warmest and saltiest water bodies in th… Mehr…
[EAN: 9783639277760], Neubuch, [PU: VDM Verlag Dr. Müller], nach der Bestellung gedruckt Neuware - Printed after ordering - The Red Sea, one of the warmest and saltiest water bodies in the world, is a recent example for ocean basin formation by break of a continent, which makes it a perfect study area to investigate the early stage of the formation of an ocean basin (e.g. magma intrusion). This book provides new data of the two sediment cores from the Shaban Deep in the northern Red Sea. Although the two cores are located about a kilometer distance, distinctly different isotopic and geochemical signals were observed. Compared to the usual stable oxygen isotope ( 18O) signatures of planktonic foraminifera in the Red Sea, a strong negative 18O shift was seen in the core 17008-1. The planktonic foraminifera shells below 183 cm core depth, showed high degrees of diagenetic alteration. This alteration has not been caused by a hydrothermal input, but rather dominated by post-depositional alteration through hot pore-waters. The heat source is most likely to be basaltic intrusion occurred before 6 ka, and located close to the core 17008-1. These results will shed light on the geological construction of the Red Sea area as well as for investigating the hydrothermal activity and ore formation in the region. 92 pp. Englisch, Books<
The Red Sea, one of the warmest and saltiest water bodies in the world, is a recent example for ocean basin formation by break of a continent, which makes it a perfect study area to inves… Mehr…
The Red Sea, one of the warmest and saltiest water bodies in the world, is a recent example for ocean basin formation by break of a continent, which makes it a perfect study area to investigate the early stage of the formation of an ocean basin (e.g. magma intrusion). This book provides new data of the two sediment cores from the Shaban Deep in the northern Red Sea. Although the two cores are located about a kilometer distance, distinctly different isotopic and geochemical signals were observed. Compared to the usual stable oxygen isotope (δ18O) signatures of planktonic foraminifera in the Red Sea, a strong negative δ18O shift was seen in the core 17008-1. The planktonic foraminifera shells below 183 cm core depth, showed high degrees of diagenetic alteration. This alteration has not been caused by a hydrothermal input, but rather dominated by post-depositional alteration through hot pore-waters. The heat source is most likely to be basaltic intrusion occurred before 6 ka, and located close to the core 17008-1. These results will shed light on the geological construction of the Red Sea area as well as for investigating the hydrothermal activity and ore formation in the region. Trade Books>Trade Paperback>Nature & Wildlife>Geology & Weather>Geology & Weather, KS OmniScriptum Publishing Core >1<
[EAN: 9783639277760], Neubuch, [PU: VDM Verlag Dr. Müller], This item is printed on demand - it takes 3-4 days longer - Neuware -The Red Sea, one of the warmest and saltiest water bodies … Mehr…
[EAN: 9783639277760], Neubuch, [PU: VDM Verlag Dr. Müller], This item is printed on demand - it takes 3-4 days longer - Neuware -The Red Sea, one of the warmest and saltiest water bodies in the world, is a recent example for ocean basin formation by break of a continent, which makes it a perfect study area to investigate the early stage of the formation of an ocean basin (e.g. magma intrusion). This book provides new data of the two sediment cores from the Shaban Deep in the northern Red Sea. Although the two cores are located about a kilometer distance, distinctly different isotopic and geochemical signals were observed. Compared to the usual stable oxygen isotope ( 18O) signatures of planktonic foraminifera in the Red Sea, a strong negative 18O shift was seen in the core 17008-1. The planktonic foraminifera shells below 183 cm core depth, showed high degrees of diagenetic alteration. This alteration has not been caused by a hydrothermal input, but rather dominated by post-depositional alteration through hot pore-waters. The heat source is most likely to be basaltic intrusion occurred before 6 ka, and located close to the core 17008-1. These results will shed light on the geological construction of the Red Sea area as well as for investigating the hydrothermal activity and ore formation in the region. 92 pp. Englisch, Books<
NEW BOOK. Versandkosten:Versandkostenfrei. (EUR 0.00) BuchWeltWeit Inh. Ludwig Meier e.K., Bergisch Gladbach, Germany [57449362] [Rating: 5 (von 5)]
[EAN: 9783639277760], Neubuch, [PU: VDM Verlag Dr. M?ller], GEOWISSENSCHAFTEN GEOLOGIE CARBONATES \\"RED-SEA\\" SAHABAN DEEP PLANKTONIC FORAMINIFERA STABLE OXYGEN ISOTOPES CARBON DIAGENESIS ALTERATION RE-MINERALIZATION SEMIOT, Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Autor/Autorin: Olgun NazliPhD student in IFM-GEOMAR (Germany). She did her bachelors in Geological Engineering in the Middle East Technical University (Turkey) and masters in University of Kiel (Germany). Her research interests cover a wide range o., Books<
[ED: Kartoniert / Broschiert], [PU: VDM Verlag Dr. Mueller], Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Autor/Autorin: Olgun NazliPhD… Mehr…
[ED: Kartoniert / Broschiert], [PU: VDM Verlag Dr. Mueller], Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Autor/Autorin: Olgun NazliPhD student in IFM-GEOMAR (Germany). She did her bachelors in Geological Engineering in the Middle East Technical University (Turkey), DE, [SC: 0.00], Neuware, gewerbliches Angebot, Hardcover, 92, [GW: 155g], 1. Auflage, Banküberweisung, PayPal<
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The Red Sea, one of the warmest and saltiest water bodies in the world, is a recent example for ocean basin formation by break of a continent, which makes it a perfect study area to investigate the early stage of the formation of an ocean basin (e.g. magma intrusion). This book provides new data of the two sediment cores from the Shaban Deep in the northern Red Sea. Although the two cores are located about a kilometer distance, distinctly different isotopic and geochemical signals were observed. Compared to the usual stable oxygen isotope (d18O) signatures of planktonic foraminifera in the Red Sea, a strong negative d18O shift was seen in the core 17008-1. The planktonic foraminifera shells below 183 cm core depth, showed high degrees of diagenetic alteration. This alteration has not been caused by a hydrothermal input, but rather dominated by post-depositional alteration through hot pore-waters. The heat source is most likely to be basaltic intrusion occurred before 6 ka, and located close to the core 17008-1. These results will shed light on the geological construction of the Red Sea area as well as for investigating the hydrothermal activity and ore formation in the region.
Detailangaben zum Buch - Holocene marine carbonate sediments in the northern Red Sea Nazli Olgun Author
Buch in der Datenbank seit 2009-03-05T07:06:33+01:00 (Berlin) Detailseite zuletzt geändert am 2023-10-31T13:40:23+01:00 (Berlin) ISBN/EAN: 9783639277760
ISBN - alternative Schreibweisen: 3-639-27776-7, 978-3-639-27776-0 Alternative Schreibweisen und verwandte Suchbegriffe: Autor des Buches: botz, reiner marks, schmidt, schmid, mark Titel des Buches: carbonate, sediment, sediments, northern northern, the deep, the sea, heat, marine nachrichtenblatt
