The DOI matches its Crossref record; 1 of the 1 references it cites were found in a registry or an index.
Kinetics of dolomitization
Abstract
Research Article| August 01, 1987 Menai Strait fault system: An early Caledonian terrane boundary in north Wales Wes Gibbons Wes Gibbons 1Department of Geology, University College, Cardiff CF1 1XL, Wales Search for other works by this author on: GSW Google Scholar Geology (1987) 15 (8): 744–747. https://doi.org/10.1130/0091-7613(1987)15<744:MSFSAE>2.0.CO;2 Article history first online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share MailTo Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Wes Gibbons; Menai Strait fault system: An early Caledonian terrane boundary in north Wales. Geology 1987;; 15 (8): 744–747. doi: https://doi.org/10.1130/0091-7613(1987)15<744:MSFSAE>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract A steep fault system runs parallel to the Menai Strait, which separates Anglesey from the mainland of north Wales. The Menai Strait fault system is interpreted as a major terrane boundary along which terrane docking took place during the late Precambrian or earliest Cambrian. The evidence is based on (1) marked geologic dissimilarities exhibited by the pre-late Early Cambrian basement to these terranes and (2) the existence of early, major ductile shear zones within the fault system. Rocks as varied as blueschists, low-grade melange, and shallow-level granitic complexes were juxtaposed along these steep shear zones prior to the eruption of ash-flow tuffs and deposition of upper Lower Cambrian marine sediments in the Welsh basin. Since the amalgamation of the Anglesey area with the Avalonian terrane (then a part of Gondwana), frequent Phanerozoic reactivation of the resulting composite terrane boundary has been restricted to mostly dip-slip fault movements. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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“Previous studies have shown that room temperature synthesis of abiotic dolomite is rarely achieved and primary (proto-)dolomite precipitation is closely associated with microbial activities.”
From Experimental evidence for abiotic formation of low-temperature proto-dolomite facilitated by clay minerals (2019) · cites this paper as Sibley et al., 1987
In the citing paper
“This hypothesis has been supported by the geological observations (e.g., poor preservation of fossils, coarse dolomite grains with dissolution pores and cavities) in dolostone and reinforced by the fact that laboratory synthesis of dolomite is difficultly achieved at Earth surface temperatures (<60 °C), whereas it is relatively uncomplicated and proceeds at a rapid rate under higher temperature di”
From Experimental evidence for abiotic formation of low-temperature proto-dolomite facilitated by clay minerals (2019) · cites this paper as Sibley et al., 1987
Citations
Cites
Revised Carbonate-water isotopic temperature scale
EPSTEIN, S., BUCHSBAUM, R., LOWENSTAM, H. A., & UREY, H. C. (1953) · Geological Society of America Bulletin · doi:10.1130/0016-7606(1953)64[1315:rcits]2.0.co;2 · Cited by 2,271
Cited by
Composition of the Continental Crust
Rudnick, R. L., & Gao, S. (2014) · Treatise on Geochemistry · doi:10.1016/b978-0-08-095975-7.00301-6 · Cited by 5,691
The geochemical evolution of the continental crust
Taylor, S. R., & McLennan, S. M. (1995) · Reviews of Geophysics · doi:10.1029/95rg00262 · Cited by 4,643
Composition of the Continental Crust
Rudnick, R. L., & Gao, S. (2003) · Treatise on Geochemistry · doi:10.1016/b0-08-043751-6/03016-4 · Cited by 3,413
Tectonic forcing of late cenozoic climate.
Raymo, M. E., & Ruddiman, W. F. (1992) · Nature · doi:10.1038/359117a0 · Cited by 2,341
Adakitic magmas: Modern analogues of Archaean granitoids
Martin, H. (1999) · Lithos · doi:10.1016/s0024-4937(98)00076-0 · Cited by 1,642
Metadata
- Authors
- Sibley, D. F., Dedoes, R. E., & Bartlett, T. R.
- Venue
- Geology
- Published
- 1987
- References
- 1
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- Sibley, D. F., Dedoes, R. E., & Bartlett, T. R. (1987). Kinetics of dolomitization. Geology. https://doi.org/10.1130/0091-7613(1987)15%3C1112%3Akod%3E2.0.co%3B2
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