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Development of columnar jointing in albite rhyolite in a rapidly cooling volcanic environment (Rupnica, Papuk Geopark, Croatia)
Author(s) -
Balen Dražen,
Petrinec Zorica
Publication year - 2014
Publication title -
terra nova
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.353
H-Index - 89
eISSN - 1365-3121
pISSN - 0954-4879
DOI - 10.1111/ter.12075
Subject(s) - rhyolite , geology , albite , lava , geochemistry , volcano , petrography , peralkaline rock , geopark , orthoclase , magma , extrusive , mineralogy , volcanic rock , feldspar , paleontology , quartz , tourism , political science , law
The Rupnica locality became the first protected geosite in Croatia in 1948 owing to a well‐exposed phenomenon of columnar jointing developed in albite rhyolite. According to the geochemical signature, melt that originated at mid‐crustal depths (10–15 km) reached a shallow emplacement level as a high‐temperature lava. Non‐destructive statistical analysis conducted at the geosite revealed that relatively narrow (29.4 ± 6.3 cm) predominantly four‐ and five‐sided columns, tightly packed striae (4.8 ± 2.1 cm) and small‐amplitude wavy sets of columns (wavelength of 32.5 ± 6.7 cm) dominate the exposed part of the Rupnica. A number of features quantified through this statistical approach, together with petrography, geochemistry and the geology of the geosite's surroundings, suggest the rapid cooling of a (sub)surface acidic lava body and the behaviour of the evolving volcanic system, developing columnar jointing under the combined influence of large‐scale constitutional supercooling and thermal contraction processes.