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pro vyhledávání: '"K. M. Gaastra"'
Autor:
H. Yang, S. M. Tikoo, C. Carvallo, D. Bilardello, P. Solheid, K. M. Gaastra, W. W. Sager, S. Thoram, K. Hoernle, T. W. Höfig, A. Avery, A. V. DelGaudio, Y. Huang, R. Bhutani, D. M. Buchs, C. Class, Y. Dai, G. Dalla Valle, S. Fielding, S. Han, D. E. Heaton, S. Homrighausen, Y. Kubota, C.‐F. Li, W. R. Nelson, E. Petrou, K. E. Potter, S. Pujatti, J. Scholpp, J. W. Shervais, M. Tshiningayamwe, X. J. Wang, M. Widdowson
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 25, Iss 2, Pp n/a-n/a (2024)
Abstract The past ∼200 million years of Earth's geomagnetic field behavior have been recorded within oceanic basalts, many of which are only accessible via scientific ocean drilling. Obtaining the best possible paleomagnetic measurements from such
Externí odkaz:
https://doaj.org/article/e0d9a459b7fa4dfa88bde9319fa158a5
