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Geochronology: Uranium-Series Dating of Ocean Formations. / Kuznetsov, Vladyslav.

Encyclopedia of Marine Geosciences. ed. / Jan Harff; Martin Meschede; Sven Petersen; Jörn Thiede. Springer Nature, 2016. p. 271-276.

Research output: Chapter in Book/Report/Conference proceeding › Chapter › Research › peer-review

Harvard

Kuznetsov, V 2016, Geochronology: Uranium-Series Dating of Ocean Formations. in J Harff, M Meschede, S Petersen & J Thiede (eds), Encyclopedia of Marine Geosciences. Springer Nature, pp. 271-276. https://doi.org/10.1007/978-94-007-6644-0_64-2

APA

Kuznetsov, V. (2016). Geochronology: Uranium-Series Dating of Ocean Formations. In J. Harff, M. Meschede, S. Petersen, & J. Thiede (Eds.), Encyclopedia of Marine Geosciences (pp. 271-276). Springer Nature. https://doi.org/10.1007/978-94-007-6644-0_64-2

Vancouver

Kuznetsov V. Geochronology: Uranium-Series Dating of Ocean Formations. In Harff J, Meschede M, Petersen S, Thiede J, editors, Encyclopedia of Marine Geosciences. Springer Nature. 2016. p. 271-276 https://doi.org/10.1007/978-94-007-6644-0_64-2

Author

Kuznetsov, Vladyslav. / Geochronology: Uranium-Series Dating of Ocean Formations. Encyclopedia of Marine Geosciences. editor / Jan Harff ; Martin Meschede ; Sven Petersen ; Jörn Thiede. Springer Nature, 2016. pp. 271-276

BibTeX

@inbook{bd1a8325de6342e1a92c908078d75491,
title = "Geochronology: Uranium-Series Dating of Ocean Formations",
abstract = "Two types of the U-series disequilibrium methods are available for dating different ocean formations and are based on radioactive (1) decay or (2) accumulation of daughter isotope. At the present time the most widespread and well-founded methods are (1) 230Thexcess, 231Paexcess, and (2) 230Th/234U and 231Pa/235U dating methods of different ocean formations. A number of ocean objects is suitable for 230Thxs and 231Paxs dating: deep-sea sediments of different origin such as carbonate (foraminiferal), silicate (radiolarian) or metalliferous sediments, and ferromanganese nodules and crusts. Both the 230Th/U and 231Pa/U methods play an important role in dating corals and mollusk shells, as well as the 230Th/U method which is most widely applied in dating seafloor massive sulfide deposits in the ocean hydrothermal zones. Modern mass spectrometric analysis allows to determine 230Thxs and 230Th/U ages between several decades to ca. 500 kyr, and 231Paxs and 231Pa/U ages up to ca. 250 kyr. Mass spectrometric measureme",
keywords = "U-series dating methods, Ocean Formations",
author = "Vladyslav Kuznetsov",
year = "2016",
doi = "10.1007/978-94-007-6644-0_64-2",
language = "English",
isbn = "978-94-007-6237-4 ",
pages = "271--276",
editor = "Harff, {Jan } and Meschede, {Martin } and Petersen, {Sven } and Thiede, {J{\"o}rn }",
booktitle = "Encyclopedia of Marine Geosciences",
publisher = "Springer Nature",
address = "Germany",

}

RIS

TY - CHAP

T1 - Geochronology: Uranium-Series Dating of Ocean Formations

AU - Kuznetsov, Vladyslav

PY - 2016

Y1 - 2016

N2 - Two types of the U-series disequilibrium methods are available for dating different ocean formations and are based on radioactive (1) decay or (2) accumulation of daughter isotope. At the present time the most widespread and well-founded methods are (1) 230Thexcess, 231Paexcess, and (2) 230Th/234U and 231Pa/235U dating methods of different ocean formations. A number of ocean objects is suitable for 230Thxs and 231Paxs dating: deep-sea sediments of different origin such as carbonate (foraminiferal), silicate (radiolarian) or metalliferous sediments, and ferromanganese nodules and crusts. Both the 230Th/U and 231Pa/U methods play an important role in dating corals and mollusk shells, as well as the 230Th/U method which is most widely applied in dating seafloor massive sulfide deposits in the ocean hydrothermal zones. Modern mass spectrometric analysis allows to determine 230Thxs and 230Th/U ages between several decades to ca. 500 kyr, and 231Paxs and 231Pa/U ages up to ca. 250 kyr. Mass spectrometric measureme

AB - Two types of the U-series disequilibrium methods are available for dating different ocean formations and are based on radioactive (1) decay or (2) accumulation of daughter isotope. At the present time the most widespread and well-founded methods are (1) 230Thexcess, 231Paexcess, and (2) 230Th/234U and 231Pa/235U dating methods of different ocean formations. A number of ocean objects is suitable for 230Thxs and 231Paxs dating: deep-sea sediments of different origin such as carbonate (foraminiferal), silicate (radiolarian) or metalliferous sediments, and ferromanganese nodules and crusts. Both the 230Th/U and 231Pa/U methods play an important role in dating corals and mollusk shells, as well as the 230Th/U method which is most widely applied in dating seafloor massive sulfide deposits in the ocean hydrothermal zones. Modern mass spectrometric analysis allows to determine 230Thxs and 230Th/U ages between several decades to ca. 500 kyr, and 231Paxs and 231Pa/U ages up to ca. 250 kyr. Mass spectrometric measureme

KW - U-series dating methods

KW - Ocean Formations

U2 - 10.1007/978-94-007-6644-0_64-2

DO - 10.1007/978-94-007-6644-0_64-2

M3 - Chapter

SN - 978-94-007-6237-4

SP - 271

EP - 276

BT - Encyclopedia of Marine Geosciences

A2 - Harff, Jan

A2 - Meschede, Martin

A2 - Petersen, Sven

A2 - Thiede, Jörn

PB - Springer Nature

ER -

ID: 7546640