The problem of genesis of berylliferous skarns

Zasedatelev, A.M.

doi:10.1080/00206817309475877

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Non-magmatic Occurrences1

Southeast China1

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1981

2022

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Cited by 5 publications

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“…Mn-Fe-oxide-rich hot spring deposits in Nevada (Golconda, Sodaville) contain up to 60 ppm Be (160 ppm BeO) along with W and other metals (Warner et al 1959). Zasedatelev (1973) suggested that similar materials occur elsewhere. Beyond a common oxide-rich, sulfide-poor geochemistry, it is not obvious that they share a common genesis.…”

Section: Non-magmatic Occurrencesmentioning

confidence: 99%

“…Central Kazakhstan pG (gr,sk) PalL (Carb L) Beus 1966, p. 293-298;Zasedatelev 1973;Burshtein 1996;Malchenko and Ermolov 1996;Serykh 1996;Dukhovskiy 2000 Be-bearing greisen and skarn deposits associated with Hercynian Be-enriched leucogranites; Mo(-W) stockwork East Qonyrat (Kounrad), Mo-W-Be-F skarn and replacement Qatpar (sk), W(-Mo) greisen Aqshantau, Qaraoba (Karaoba); unnamed Magmica-Fl-Ch Aqshatau, Kazakhstan (see Fig. 17)…”

Section: Southeast Chinamentioning

confidence: 99%

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