Diagenesis and shear rheology of a Recent-Pleistocene volcanogenic sequence, Mexican Basin. Implications to swelling and stability
Low-grade diagenesis in the Recent-Pleistocene volcanogenic sequence of the Mexican Basin formed, in the gravel and sand strata, kaolinite, smectite and interstratified kaolinite/smectite, intimately associated with fine ash containing volcanic glass, opal-C, plagioclase, K-feldspar and pyroxene, i...
I tiakina i:
| Ngā kaituhi matua: | , , |
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| Hōputu: | Artigo |
| Reo: | Inglês |
| I whakaputaina: |
Universidad Nacional Autónoma de México
2018-06-01
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| Rangatū: | Revista Mexicana de Ciencias Geológicas |
| Ngā marau: | |
| Urunga tuihono: | https://rmcg.unam.mx/index.php/rmcg/article/view/993 |
| Ngā Tūtohu: |
Kāore He Tūtohu, Me noho koe te mea tuatahi ki te tūtohu i tēnei pūkete!
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