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Autor:
C Claoué
Sir, I was illuminated to read the RCOphth eponymous lecture in the October issue of Eye.1 However, I was disappointed that it compounds the confusion regarding the correct name of the condition. Although the disease is called “Fuchs dystrophy” f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2bff6a0116a9e95e8ef3c5cbe3da1421
https://europepmc.org/articles/PMC4017109/
https://europepmc.org/articles/PMC4017109/
Publikováno v:
Marine and Petroleum Geology. 18:319-337
The understanding of sediment provenance and sediment transport routes is a key element in establishing reservoir presence in clastic petroleum systems. Determination of sediment provenance is particularly difficult in structurally complex areas and
Publikováno v:
Geological Society of America Bulletin. 112:1315-1341
Defining and dating the base of the Kiaman (the long period of reverse polarity that spans the time from the Late Carboniferous to the middle Permian) have proven difficult. In an attempt to do this an integrated stratigraphic, paleomagnetic, and geo
Publikováno v:
Australian Journal of Earth Sciences. 44:535-538
SHRIMP zircon dates from Permian ignimbrites and tuffs associated with fossiliferous strata within the Sydney‐Bowen Basin and New England Orogen are used to establish a time scale for the Permian System in eastern Australia. For the first time this
Publikováno v:
Journal of the Geological Society. 153:915-929
Detrital zircons in sandstones of the Statfjord Formation (late Triassic-early Jurassic) in the northern North Sea have been dated with the sensitive high resolution ion microprobe (SHRIMP). These sandstones lack detailed biostratigraphic control, bu
Publikováno v:
Australian Journal of Earth Sciences. 43:401-421
Publikováno v:
Geological Society, London, Special Publications. 89:145-174
Publikováno v:
Geological Magazine. 129:281-291
The SHRIMP ion microprobe has been used to date zircons in a 1 cm thick bentonite located in the Hasselbachtal auxiliary global stratotype section through the Devonian-Carboniferous boundary in Germany, and a tuff located at a similar biostratigraphi