Using <sup>87</sup>Sr/<sup>86</sup>Sr LA-MC-ICP-MS Transects within Modern and Ancient Calcite Crystals to Determine Fluid Flow Events in Deep Granite Fractures
The strontium isotope signature (<sup>87</sup>Sr/<sup>86</sup>Sr) of calcite precipitated in rock fractures and faults is a frequently used tool to trace paleofluid flow. However, bedrock fracture networks, such as in Precambrian cratons, have often undergone multiple fractur...
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| 格式: | 文件 |
| 语言: | English |
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MDPI AG
2020-09-01
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| 丛编: | Geosciences |
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| 在线阅读: | https://www.mdpi.com/2076-3263/10/9/345 |