Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms
Volume 29, Issues 1–2, 2 November 1987, Pages 322-325
Beryllium-10 data from redeposited late miocene pelagic sediments (East Java, Indonesia)
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Cited by (1)
Beryllium-10 in Australasian tektites: Constraints on the location of the source crater
2004, Geochimica et Cosmochimica ActaCitation Excerpt :Again, higher 10Be concentrations in paleosols are apparent, and within layers, two-to-three fold variations of 10Be concentrations are common over depth ranges of less than 10 m. The bottom panel of Figure 3 shows results from De Boer et al. (1987), who analyzed 10Be in “Late Miocene to Early Pliocene (6–3 Ma BP) pelagic carbonates exposed along the Solo River, north of the city of Ngawi, East Java (Indonesia)” (7°S, 111°E). Samples are described as marly pelagic fine-grained mixed carbonate/clayey sediments and as coming from heights ranging from 0 to 320 m. Those authors remarked that, “On a smaller scale the 10Be data show strong deviations, up to a factor of 1.7 between adjacent samples.”
Copyright © 1987 Published by Elsevier B.V.