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Rates of Tectonometamorphic Processes from Rubidium and Strontium Isotopes in Garnet

Christensen, John N., Rosenfeld, John L., DePaolo, Donald J.·1989·Science

Abstract

Measurement of the radial variation of the 87 Sr/ 86 Sr ratio in a single crystal from a metamorphic rock can be used to determine the crystal's growth rate. That variation records the accumulation of 87 Sr from radioactive decay of 87 Rb in the rock matrix from which the crystal grew. This method can be used to study the rates of petrological processes associated with mountain building. It is applied to garnet crystals in rocks from southeast Vermont that were metamorphosed about 380 million years ago. The average growth rate measured for three garnets is 1.4 -0.45 +0.92 millimeters per million years and the average time interval of growth is 10.5 ± 4.2 million years. Garnet and its mineral inclusions provide a sequential record of temperature change, strain, and chemical reactions during metamorphism; therefore, the technique offers the potential for determination of the rates of those processes as well. The growth interval and observed amount of rotation recorded by inclusion trails in one garnet indicate that the mean shear strain rate during garnet growth was 2.4 -0.7 +1.6 × 10 -14 per second.

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Metadata

Authors
Christensen, J. N., Rosenfeld, J. L., & DePaolo, D. J.
Venue
Science
Published
1989-06-23
Volume
244
Issue
4911
Pages
1465-1469
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2040012572
Cited by
312
References
0
FWCI
7.47
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Rates of Tectonometamorphic Processes from Rubidium and Strontium Isotopes in Garnet. https://app.cochat.ai/papers/10.1126/science.244.4911.1465
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Christensen, J. N., Rosenfeld, J. L., & DePaolo, D. J. (1989). Rates of Tectonometamorphic Processes from Rubidium and Strontium Isotopes in Garnet. Science. https://doi.org/10.1126/science.244.4911.1465

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