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Cited by 425

The DOI matches its Crossref record; 37 of the 37 references it cites were found in a registry or an index.

Himalayan Tectonics, Weathering Processes, and the Strontium Isotope Record in Marine Limestones

Edmond, J. M.·1992·Science

Abstract

The time evolution of the isotopic composition of seawater strontium (the ratio of strontium-87 to strontium-86) over the last 500 million years has the form of an asymmetric trough. The values are highest in the Cambrian and Recent (0.7091) and lowest in the Jurassic (0.7067). Superimposed on this trend are a number of smaller oscillations. Consideration of the geochemical cycle of strontium and the dynamics of weathering shows that only Himalayan-style continental collisions can influence the isotope ratio on the scale observed. The contemporary Himalayan orogeny is by far the largest since the late Precambrian Pan-African event that produced the high in the Cambrian.

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Metadata

Authors
Edmond, J. M.
Venue
Science
Published
1992-12-04
Volume
258
Issue
5088
Pages
1594-1597
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W1988997369
Cited by
425
References
37
FWCI
18.89
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Himalayan Tectonics, Weathering Processes, and the Strontium Isotope Record in Marine Limestones. https://app.cochat.ai/papers/10.1126/science.258.5088.1594
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Edmond, J. M. (1992). Himalayan Tectonics, Weathering Processes, and the Strontium Isotope Record in Marine Limestones. Science. https://doi.org/10.1126/science.258.5088.1594

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.