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In the Kodiak accretionary complex, Kodiak Island, Alaska, pseudotachylyte occurs in black, locally vitreous ultrafine-grained fault rock. Microscopic observations show that the pseudotachylytes are composed of glass, with vesicles, amygdules, microl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::796b8c08b6cddf7aa0fd5d0c9d9535c6
http://hdl.handle.net/11568/786569
http://hdl.handle.net/11568/786569
