Abstract Natural hydrous silicas may be subdivided into three well‐defined structural groups—opal‐C (well‐ordered α‐cristobalite), opal‐CT (disordered a‐cristobalite, a‐tridymite) and opal‐A (highly disordered, near amorphous). Lussatite from the original locality is identical with opal‐CT and thus appears to be a legitimate term for this class of opal. Although the prime criterion used is the nature of…
Journal of the Geological Society of Australia Template
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About the Journal of the Geological Society of Australia format
Journal of the Geological Society of Australia is a peer-reviewed journal published by Taylor & Francis, covering Geological and Geochemical Analysis, Geological and Geophysical Studies, Geology and Paleoclimatology Research.
| Publisher | Taylor & Francis |
|---|---|
| Reference style | Author–year (Chicago, T&F) Author–year — (Smith, 2023) in the text Smith, Ada, Ben Jones, and Cara Lee. 2023. "A Representative Article Title." Journal of the Geological Society of Australia 12 (3): 45–58.
Formats any DOI in Journal of the Geological Society of Australia style. No sign-up. |
| Publishes research in | Geological and Geochemical Analysis Geological and Geophysical Studies Geology and Paleoclimatology Research Geochemistry and Geologic Mapping Geological formations and processes |
| ISSN | 0016-7614 |
| h-index | 66 |
| i10-index | 499 |
| Total citations | 20,581 |
| Top institutions publishing here | Australian National University |
| Journal website | www.tandfonline.com |
| You get | A submission-ready PDF and the editable LaTeX source — ready to submit. |
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Most-cited papers in Journal of the Geological Society of Australia
Abstract Two distinct groups of granitoids occur on the eastern side of the Kosciusko Batholith. Those considered to be derivatives of sedimentary source rocks (S‐types) are usually foliated and either contain cordierite or white‐mica secondary after cordierite. The granitoids produced from igneous source material (I‐types) are generally massive and frequently contain hornblende. Geochemical parameters provide…
Abstract Archaean gold deposits of Australia are most abundant in 2.8 ± 0.1 Ga granitoid‐greenstone terrains, where they form both vein‐type and disseminated occurrences. Two‐thirds of total gold production has come from metamorphic (early, peak or late) vein deposits within host rocks of metabasaltic composition and of greenschist to lower amphibolite facies grade. Wallrock alteration,…
Abstract From the results of this preliminary survey it would appear that the bathyliths of the southern belt of the Tasman Geosyncline represent a history of continuous tectonic activity from Middle Silurian through to Middle Devonian, with a gradual movement eastwards of the axis of the intrusions. The gneissic “Ordovician‐type” granite is dominant in the…
Abstract During the Cainozoic there was widespread volcanism, mainly basaltic, in eastern New South Wales. Numerous new K‐Ar ages, together with previously published results, provide information on the age of virtually all the main volcanic provinces, and indicate that the volcanism started about 70 m.y. ago in the Late Cretaceous, and was continuous from about…