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Geology of the Rakiraki district, Viti Levu, Fiji

TLDR
The area west and south-west of Rakiraki, Fiji is composed of basaltic and andesitic flows, fragmental and pillow lavas intruded by andesite plugs, a gabbro pluton, and dikes as mentioned in this paper.
Abstract
The area west and south-west of Rakiraki, Fiji, is composed of basaltic and andesitic flows, fragmental and pillow lavas intruded by andesitic plugs, a gabbro pluton, and andesitic dikes. The area was a major volcanic centre in Pliocene-Pleistocene times. The stratigraphy and petrology are discussed.

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Early rifting of an oceanic island arc (Fiji) produced shoshonitic to tholeiitic basalts

TL;DR: In this article, three shoshonitic suites are distinguished based on differentiation-normalized alkali contents, but K-Rb-Ba-Sr, P-rare earth element (REE), and Ti-Zr-Hf enrichments occur independent of each other.
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Characteristics and origin of peperite involving coarse-grained host sediment

TL;DR: Peperite involving basalt and polymictic volcanic conglomerate occurs in the Pliocene Ba Volcanic Group at Yaqara in northern Viti Levu, Fiji as mentioned in this paper.
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Volcano-tectonic evolution of Fiji and adjoining marginal basins

TL;DR: In this article, a compressive event followed by progressive isolation from a subduction regime as arc segments were rotated away from the region led to asthenospheric melting with a decreasing subduction component, and a consequent change in Fiji volcanism from arc andesites and tholeiites to alkalic ocean island basalts.
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Petrography and geologic provenance of sand tempers in prehistoric potsherds from Fiji and Vanuatu, South Pacific

TL;DR: In this article, the authors have found evidence for prehistoric ceramic transfer between Vanuatu and Fiji, but there is as yet no temper evidence for such transfer between islands of origin.
References
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Rock-forming minerals

Journal ArticleDOI

Average chemical compositions of some igneous rocks

TL;DR: In this paper, the average chemical compositions for the common plutonic rock types and their volcanic equivalents are given for the general average chemical composition of silicic, intermediate, subsilicic and ultramafic igneous rocks.
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The Petrology of Thingmuli, a Tertiary Volcano in Eastern Iceland

TL;DR: The Tertiary flood-basalt sequence of eastern Iceland is intermittently disturbed by central volcanic activity with the voluminous eruption of acid magma as mentioned in this paper, which produces a swarm of acid and basic dykes and extensive superimposed hydrothermal alteration.
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Proposed classification of volcaniclastic sediments and rocks

TL;DR: In this paper, the authors classified volcanic sediments and rocks into three classes: autoclastic, pyroclastic, and epiclastic, with grain-size limits the same as non-volcanic volcanic rocks.
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Pahoehoe, aa, and block lava

TL;DR: Macdonald as discussed by the authors describes the surface features and cross-sections of pahoehoe and aa and concludes that aa has the same chemistry and viscosity as aa, but has lost gas, such that agitation or stirring of the lava is important in effecting the transition from aa to aa.
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