nd si n F release of Hf and Pb isotopes. The modelled Nd isotopes imply a relative decrease in water mass advection into the Labrador Sea 2 Radiogenic isotopes of elements with long oceanic (Nd), hafnium (Hf), and lead (Pb), preserve regional variations that reflect local erosional sources and their...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.531.6614 2023-05-15T17:06:00+02:00 The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.531.6614 http://www.geomar.de/fileadmin/personal/fb1/p-oz/mfrank/Reynolds_et_al_2006_chem_geol.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.531.6614 http://www.geomar.de/fileadmin/personal/fb1/p-oz/mfrank/Reynolds_et_al_2006_chem_geol.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.geomar.de/fileadmin/personal/fb1/p-oz/mfrank/Reynolds_et_al_2006_chem_geol.pdf Weathering Isotope geochemistry Radiogenic isotopes Glacial erosion Argon–argon text ftciteseerx 2016-01-08T10:38:17Z nd si n F release of Hf and Pb isotopes. The modelled Nd isotopes imply a relative decrease in water mass advection into the Labrador Sea 2 Radiogenic isotopes of elements with long oceanic (Nd), hafnium (Hf), and lead (Pb), preserve regional variations that reflect local erosional sources and their rculation (Albarede Chemical Geology 226 (200between 2.4 and 1.5 Ma, accompanied by a decrease in the rate of overturning, possibly caused by an increased freshwater input into the Labrador Sea. Text Labrador Sea Unknown |
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Open Polar |
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Unknown |
op_collection_id |
ftciteseerx |
language |
English |
topic |
Weathering Isotope geochemistry Radiogenic isotopes Glacial erosion Argon–argon |
spellingShingle |
Weathering Isotope geochemistry Radiogenic isotopes Glacial erosion Argon–argon |
topic_facet |
Weathering Isotope geochemistry Radiogenic isotopes Glacial erosion Argon–argon |
description |
nd si n F release of Hf and Pb isotopes. The modelled Nd isotopes imply a relative decrease in water mass advection into the Labrador Sea 2 Radiogenic isotopes of elements with long oceanic (Nd), hafnium (Hf), and lead (Pb), preserve regional variations that reflect local erosional sources and their rculation (Albarede Chemical Geology 226 (200between 2.4 and 1.5 Ma, accompanied by a decrease in the rate of overturning, possibly caused by an increased freshwater input into the Labrador Sea. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
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Text |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.531.6614 http://www.geomar.de/fileadmin/personal/fb1/p-oz/mfrank/Reynolds_et_al_2006_chem_geol.pdf |
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Labrador Sea |
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Labrador Sea |
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http://www.geomar.de/fileadmin/personal/fb1/p-oz/mfrank/Reynolds_et_al_2006_chem_geol.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.531.6614 http://www.geomar.de/fileadmin/personal/fb1/p-oz/mfrank/Reynolds_et_al_2006_chem_geol.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766060898082881536 |