10Be contents of late Cenozoic sediments from Sites 720, 722, and 728 in the western Arabian Sea

C. J. Beets; G. T. Klaver; D. Kroon; K. Van Der Borg; A. F.M. De Jong

¹⁰Be contents of late Cenozoic sediments from Sites 720, 722, and 728 in the western Arabian Sea

C. J. Beets, G. T. Klaver, D. Kroon, K. Van Der Borg, A. F.M. De Jong

Earth and Climate

Research output: Contribution to Journal › Article › Academic › peer-review

Abstract

Differences in scavenging intensity and upwelling in the water column, must account for the variations in the initial ¹⁰Be input into the sediments from Holes 728A and 722A, whereas differences in sediment character and sedimentation rate can explain the variances between Holes 722A, 728A, and 720A. -from Authors

Original language	English
Pages (from-to)	455-458
Number of pages	4
Journal	Proceedings of the Ocean Drilling Program. Scientific Results
Publication status	Published - 1 Jan 1991

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title = "10Be contents of late Cenozoic sediments from Sites 720, 722, and 728 in the western Arabian Sea",

abstract = "Differences in scavenging intensity and upwelling in the water column, must account for the variations in the initial 10Be input into the sediments from Holes 728A and 722A, whereas differences in sediment character and sedimentation rate can explain the variances between Holes 722A, 728A, and 720A. -from Authors",

author = "Beets, {C. J.} and Klaver, {G. T.} and D. Kroon and {Van Der Borg}, K. and {De Jong}, {A. F.M.}",

year = "1991",

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journal = "Proceedings of the Ocean Drilling Program. Scientific Results",

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AU - Beets, C. J.

AU - Klaver, G. T.

AU - Kroon, D.

AU - Van Der Borg, K.

AU - De Jong, A. F.M.

PY - 1991/1/1

Y1 - 1991/1/1

N2 - Differences in scavenging intensity and upwelling in the water column, must account for the variations in the initial 10Be input into the sediments from Holes 728A and 722A, whereas differences in sediment character and sedimentation rate can explain the variances between Holes 722A, 728A, and 720A. -from Authors

AB - Differences in scavenging intensity and upwelling in the water column, must account for the variations in the initial 10Be input into the sediments from Holes 728A and 722A, whereas differences in sediment character and sedimentation rate can explain the variances between Holes 722A, 728A, and 720A. -from Authors

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ER -

¹⁰Be contents of late Cenozoic sediments from Sites 720, 722, and 728 in the western Arabian Sea

Abstract

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