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The upper mantle beneath Patagonia, Argentina, documented by xenoliths from alkali basalts

Autor: Bjerg, E.A. ^*, Ntaflos, T., Kurat, G., Dobosi, G., Labudía, C.H.

Publikováno v: In Journal of South American Earth Sciences 2005 18(2):125-145

Geometric analysis and timing of structures on mafic–ultramafic bodies and high grade metamorphic rocks in the Sierras Grandes of San Luis Province, Argentina

Autor: Delpino, S.H. ^*, Dimieri, L., Bjerg, E.A., Kostadinoff, J., Mogessie, A., Hoinkes, G., Hauzenberger, Ch.A., Felfernig, A.

Publikováno v: In Journal of South American Earth Sciences April 2001 14(1):101-112

Combining the SHAP Method and Machine Learning Algorithm for Desert Type Extraction and Change Analysis on the Qinghai–Tibetan Plateau.

Autor: Lu, Ruijie¹ (AUTHOR) luruijie@nieer.ac.cn, Liu, Shulin¹ (AUTHOR) liusl@lzb.ac.cn, Duan, Hanchen¹ (AUTHOR), Kang, Wenping¹ (AUTHOR), Zhi, Ying^1,2 (AUTHOR)

Publikováno v: Remote Sensing. Dec2024, Vol. 16 Issue 23, p4414. 30p.

Spinel group minerals in metamorphosed ultramafic rocks from Río de Las Tunas belt, Central Andes, Argentina

Autor: GARGIULO, M.F., BJERG, E.A., MOGESSIE, A.

Publikováno v: Geologica Acta; 2013: Vol.: 11 Núm.: 2; p. 133-148
Geologica Acta; Vol. 11 No 2 (2013); 133-148
Geologica Acta; Vol. 11 No. 2 (2013); 133-148
Geologica Acta; Vol. 11 Núm. 2 (2013); 133-148
RCUB. Revistas Científicas de la Universidad de Barcelona
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Dipòsit Digital de Documents de la UAB
Universitat Autònoma de Barcelona

In the Río de Las Tunas belt, Central Andes of Argentina, spinel group minerals occur in metaperidotites and in reaction zones developed at the boundary between metaperidotite bodies and their country-rocks. They comprise two types: i) Reddish-brown

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::3a03af0f61d0ba43066afa75c0587b86
http://www.raco.cat/index.php/GeologicaActa/article/view/265919