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Opal-CT from
Suba quarry, Király Hill, Mád, Szerencs District, Borsod-Abaúj-Zemplén County, Hungary


Locality type:Quarry
Classification
Species:Opal var: Opal-CT
Formula:SiO2 · nH2O
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Opal-CT data
Locality Data:Click here to view Suba quarry, Király Hill, Mád, Szerencs District, Borsod-Abaúj-Zemplén County, Hungary
Data Identifiers
Mindat Occurrence Record ID:1315539
Long-form Identifier:1:3:1315539:1
GUID (UUID V4):07400537-e007-4072-b19b-9c032a6b1009
References
Reference Search (possible matching items)
Book
(1972) Origin of the Mormon Mesa Caliche, Clark County, Nevada. Geol Soc Arn Bu ll 83:143-155 Gauthier-Lafaye...ooo tons) is located at the top of a 380-m-high hill (Morit Tato). The profile displays an isalterite...15 m requires 45 m of granite on the top of the hill where lateral accumulations are not expected (Boulange...which develop from the bottom to the top of the hill, contribute to the levelling of the landscape (Boulange...Disequilibri um (Transformation Systems) 79 RESIDUAL HILL WI TH OISMANTLEO IRONCRUST or less LJ More differentiated
Book
available (as from the C-Thru Ruler Co., Bloomfield, CT 06002). Sets of 6-in. scales graduated in various...p ..<.. . ________ , F ie. l.d. .. .!b.e-.eJ:. .:ct. 3 .,..c .ont._ _1 hrst- _ .$py_r .... NIIl of...Isaacs brief, the hydrated amorphous form of SiOz (opal-A) makes 1982{-t1nns of diatoms, radiolarians, and...transsk~ ~ ~layered cristobalite and tridymite (opa!-CT) at temperat ures t:~~t~ about 750 m of burial. A...stone ' transform s to quartz at temperat ·a1 oopal-CT · to ures correspondmg burt ' · usua II y ch a1ce
Book
addition, productivity of biogenic carbonate and opal may significantly vary from glacial to interglacial...layers in subaqueous environments. Ash layers on hill slopes may be incorporated into periglacial processes...CARBONATE BUILDUP C1 FALLING SEA-LEVEL INTENSIVE CT MEDIUM LITTLE K ARSTIFICA TlON Fig. 3.25. a Complete...sediment composition fluctuated from carbonate-rich to opal-rich sections. Intensified bottom water circulation...between about 30 and 75 % of the total amount of opal-concentrating organisms, in Antarctic waters 99
 
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