Decoding Earth's plate tectonic history using sparse geochemical data
Abstract
Accurately mapping plate boundary types and locations through time is essential for understanding the evolution of the plate-mantle system and the exchange of material between the solid Earth and surface environments. However, the complexity of the Earth system and the cryptic nature of the geological record make it difficult to discriminate tectonic environments through deep time. Here we present a new method for identifying tectonic paleo-environments on Earth through a data mining approach using global geochemical data. We first fingerprint a variety of present-day tectonic environments utilising up to 136 geochemical data attributes in any available combination. A total of 38301 geochemical analyses from basalts aged from 5–0 Ma together with a well-established plate reconstruction model are used to construct a suite of discriminatory models for the first order tectonic environments of subduction and mid-ocean ridge as distinct from intraplate hotspot oceanic environments, identifying 41, 35, and 39 key discriminatory geochemical attributes, respectively. After training and validation, our model is applied to a global geochemical database of 1547 basalt samples of unknown tectonic origin aged between 1000–410 Ma, a relatively ill-constrained period of Earth's evolution following the breakup of the Rodinia supercontinent, producing 56 unique global tectonic environment predictions throughout the Neoproterozoic and Early Paleozoic. Predictions are used to discriminate between three alternative published Rodinia configuration models, identifying the model demonstrating the closest spatio-temporal consistency with the basalt record, and emphasizing the importance of integrating geochemical data into plate reconstructions. Our approach offers an extensible framework for constructing full-plate, deep-time reconstructions capable of assimilating a broad range of geochemical and geological observations, enabling next generation Earth system models.
Additional Information
© 2019 China University of Geosciences (Beijing) and Peking University. Production and hosting by Elsevier B.V. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/). Received 10 October 2018, Revised 18 March 2019, Accepted 9 May 2019, Available online 17 May 2019. This research was supported by the Science Industry Endowment Fund (RP 04-174) Big Data Knowledge Discovery Project. MGT received additional support from a CSIRO-Data61 Postgraduate Scholarship. ZXL acknowledges the support of the Australian Research Council through a Laureate Fellowship grant (FL150100133). We thank Derrick Hasterok and an anonymous reviewer for their considered and constructive reviews, Craig O'Neill, Peter Cawood, Thomas Bodin and Andrew Merdith for helpful comments that improved the paper, and Jason Ash and Daniel Steinberg for their combined technical support in developing these analyses. This is a contribution to IGCP project 648. Analyses were conducted using the following open source tools: GPlates and pyGPlates (www.gplates.org), Python (www.python.org), and Project Jupyter (www.jupyter.org).Attached Files
Published - 1-s2.0-S1674987119300908-main.pdf
Supplemental Material - 1-s2.0-S1674987119300908-mmc1.pdf
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Additional details
- Eprint ID
- 95562
- Resolver ID
- CaltechAUTHORS:20190517-100807069
- Science and Industry Endowment Fund
- RP 04-174
- Commonwealth Scientific and Industrial Research Organisation (CSIRO)
- Australian Research Council
- FL150100133
- Created
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2019-05-17Created from EPrint's datestamp field
- Updated
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2021-11-16Created from EPrint's last_modified field
- Caltech groups
- Seismological Laboratory