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Sm-Nd Isotope Data Compilation from Geoscientific Literature Using an Automated Tabular Extraction Method
Zhixin Guo1,2,3,4, Tao Wang5, Chaoyang Wang5
1Shanghai Jiao Tong University, School of Electronic Information and Electrical Engineering, Shanghai, 200240, China.
This study introduces an automated method to extract rare earth element data (Samarium-Neodymium) from geoscience literature, improving crustal evolution research. The approach efficiently compiles scattered data, enhancing scientific knowledge accessibility.
Area of Science:
- Geochemistry
- Isotope Geology
- Earth Sciences
Background:
- Rare earth elements Samarium (Sm) and Neodymium (Nd) are vital for understanding crustal growth and evolution.
- The Sm-Nd isotopic system is key for determining crustal formation ages due to element immobility during metamorphism.
- Geoscience data on Sm-Nd are fragmented across literature, hindering comprehensive analysis.
Purpose of the Study:
- To develop an automated method for extracting tabular geoscience data, specifically Sm-Nd isotopic data.
- To overcome challenges of scattered data and improve efficiency in data acquisition for earth science research.
Main Methods:
- An automated tabular extraction technique was employed to harvest Sm-Nd data from geoscience publications.
- Data were collected from 9,138 tables across over 20,000 publications, yielding 10,624 Sm-Nd data entries.
- A subset of 2,118 data points was manually curated to augment existing global datasets.
Main Results:
- Successfully collected over 10,000 Sm-Nd data entries using the automated method.
- Significantly increased the size of the global Sm-Nd dataset by over 20% with curated data.
- Demonstrated the efficiency and scalability of the automated data collection methodology.
Conclusions:
- Automated data extraction significantly enhances the efficiency of acquiring critical geoscience data.
- This methodology provides a scalable solution for compiling fragmented datasets across various scientific domains.
- Improved data accessibility facilitates more robust research into fundamental questions of crustal evolution.
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