Results 11 to 20 of about 5,229 (211)
Experimental Constraints on the Origin of the 1991 Pinatubo Dacite [PDF]
Crystallisation and mantle-interaction experiments have been performed on the 1991 Pinatubo dacite to constrain its petrogenesis. In the dacite- H2O system at 1000 MPa, magnetite and either clinopyroxene or amphibole are the liquidus phases. No garnet is observed at this pressure.
Prouteau, Gaëlle, Scaillet, Bruno
core +11 more sources
Ruby Xenocrystals in Dacite from Central Mexico [PDF]
The occurrence of 1-2 cm in diameter, anhedral xenocrystals of red corundum (ruby) in a dacitic lava- flow from central Mexico -in the state of Hidalgo- has been recorded. Geochemically, this dacite nearly resembles adakitic rock (SiO2=63.73 66.64 wt %),
Luis Enrique Ortiz Hernández +1 more
doaj +3 more sources
The hydration reaction of mass concrete seriously endangers the structural safety. At present, the concrete production relies excessively on fly ash due to hydration reaction.
Lu Liu +7 more
doaj +2 more sources
The characteristics and morphology of columnar dacite in Tawau, Sabah [PDF]
The occurrence of columnar jointing is commonly associated with volcanic rocks and a rapid cooling environment. We recently discovered well-preserved columnar dacite on the road cutting slope in the eastern part of Tawau town, Sabah.
James, Elvaene +4 more
openaire +3 more sources
Discovery of basaltic and magnesian andesite magmas within the Hunga volcanic system, Tonga arc [PDF]
The climactic explosive eruption of Hunga volcano in January 2022 destroyed a significant portion of the Hunga Tonga-Hunga Ha’apai islands, deepening the caldera floor by over 600 m and depositing 3.5 km3 of material onto its submarine flanks.
Yoshihiko Tamura +8 more
doaj +2 more sources
This study used the indexes of fineness, pozzolanic activity, hydration heat, mortar fluidity and strength, and circular cracking degree, and combined the techniques of SEM, EDS, XRD, MIP, and TG-DSC.
Zheyuan Liu, Juhong Han, Liangjian Hu
doaj +2 more sources
In the surveyed area, so-called Tamagawa Dacites are largely divided into three parts. The lower part of the Tamagawa Dacites is an alternation of dacitic tuff, lapilli tuff, tuff breccia, volcanic breccia, tuffaceous sandstone and siltstone (T1), accompanied by an alternation of siltstone and tuff (T2) on ascending order.
Orimoto, Sachio, Yasuda, Tadashi
openaire +2 more sources
The age of undeformed dacite intrusions within the Kolaka Fault zone, SE Sulawesi, Indonesia [PDF]
We present petrologic, geochemical and U–Pb sensitive high resolution ion microprobe (SHRIMP) data from previously undocumented dacite intrusions from the SE Arm of Sulawesi.
White, Lloyd +2 more
core +1 more source
Role of crustal assimilation in the evolution of andesitic and dacitic magmas from Makran volcanic arc with special reference to Pb isotopes [PDF]
Introduction The Makran volcanic arc in southern Iran is one of the few active ocean-continent subduction systems in the Alp-Himalaya orogen (Priestley et al., 2021). It includes four volcanic fields: Shahsavaran (SVF), Bazman (BVF), west of Khash (KVF),
Zahra Firouzkouhi, Ali Ahmadi
doaj +1 more source
In the northwestern Korean Peninsula, Cretaceous volcanic rocks are composed of andesite, andesite-dacite and rhyolite intercalated with terrigenous clastic rocks.
Jonghyok Yang +11 more
doaj +1 more source

