Growth fault control of Early Archaean cherts, barite mounds and chert-barite veins, North Pole Dome, Eastern Pilbara, Western Australia
References (55)
- et al.
Filamentous fossil bacteria from the Archean of Western Australia
Precam. Res.
(1983) - et al.
Carbonaceous filaments from North Pole, Western Australia: are they fossil bacteria in Archean stromatolites?
A discussion
Precam. Res.
(1988) Volcanic, sedimentary and tectonostratigraphic environments of the ∼ 3,46 Ga Warrawoona Megasequence: a review
- et al.
Sedimentary evidence for an Archean shallow-water volcanic-sedimentary facies, Eastern Pilbara Block, Western Australia
Earth Planet. Sci. Lett.
(1979) - et al.
Horizontal tectonics pre-dating upper Gorge Creek Group sedimentation, Pilbara Block, Western Australia
Precam. Res.
(1987) Carbonaceous filaments from North Pole, Western Australia: are they fossil bacteria in Archaean stromatolites
Precam. Res.
(1984)Carbonaceous filaments from the North Pole, Western Australia: are they fossil bacteria in Archacan stromatolites?
A reply
Precam. Res.
(1988)- et al.
Stratigraphy and sedimentology of an early ARchean felsic volcanic sequence, eastern Pilbara Block, Western Australia, with special reference to the Duffer Formation and implications for crustal evolution
Precam. Res.
(1989) Brittle microtectonics: principles and practice
J. Struct. Geol.
(1985)Sequence stratigraphy of the Archaean supracrustal belts of the Pilbara Block, Western Australia
Sedimentology of the Middle Marker (3.4 Ga), Onverwacht Group, Transvaal, South Africa
Precam. Res.
Restricted shallow-water sedimentation of early Archean stromatolithic and evaporitic strata of the Strelley Pool Chert, Pilbara Block, W.A.
Precam. Res.
Constraints on the age of the Warrawoona Group, eastern Pilbara Block, Western Australia
Geochemical characteristics of Archean cherts and other sedimentary rocks in the Pilbara Block, Western Australia: evidence for Archean seawater enriched in hydrothermally-derived iron and silica
Precam. Res.
U Pb zircon geochronology of Archaean felsic units in the Marble Bar region, Pilbara Craton, Western Australia
Precam. Res.
Evidence for multiphase deformation in the Archean basal Warrawoona Group in the Marble Bar area, East Pilbara, Western Australia
Precam. Res.
New fossil finds in old rock
Nature
Volcanism and hydrothermal alteration, Warrawoona Group, East Pilbara
A review of Archean volcanic-hosted massive sulphide and sulphate mineralization in Western Australia
Econ. Geol.
Submarine barite-opal rocks of hydrothermal origin
Science
Life and conditions in the early Archaean: evidence from 3500 m.y. old shallow-water sediments in the Warrawoona Group, North Pole, Western Australia
Microfossil recognition in Archean rocks: an appraisal of spheroids and filaments from a 3500 m.y. old chert-barite unit at North Pole, Western Australia
Palaios
Cherts in the Warrawoona Group: Early Archaean silicified sediments deposited in shallow-water environments
Evaporitic sediments of early Archean age from the Warrawoona Group, North Pole, W.A.
Sedimentology
Stromatolite recognition in ancient rocks: an appraisal of irregular laminated structures in an early Archaean chert-barite unit from North Pole, Western Australia
Alcheringa
Record of emergent continental crust ∼ 3.5 billion years ago in the Pilbara craton of Australia
Nature
Submarine volcanism: eruption styles, products, and relevance to understanding the host-rock successions to volcanic-hosted massive sulphide deposits
Econ. Geol.
Cited by (109)
Early Archean biogeochemical iron cycling and nutrient availability: New insights from a 3.5 Ga land-sea transition
2022, Earth-Science ReviewsCitation Excerpt :Given our focus on jaspilites, no samples from A2 were taken. The syn-depositional nature of many of the chert-barite veins support the volcanic caldera model put forth for the Dresser Formation lower chert-barite sequence (Nijman et al., 1998; Van Kranendonk et al., 2008, 2019a; Tadbiri and Van Kranendonk, 2020), and provide important constraints on hydrothermal fluid compositions. It is expected that Fe in the A1 jaspilites should reflect local sources, either from the deep, local vein system, or from surface water runoff, given the inferred lacustrine or restricted depositional conditions indicated by their restricted lateral occurrence.
Life analog sites for Mars from early Earth: diverse habitats from the Pilbara Craton and Mount Bruce Supergroup, Western Australia
2021, Mars Geological Enigmas: From the Late Noachian Epoch to the Present Day
- 1
Present address: Netherlands Research School of Sedimentary Geology, Free University, Amsterdam. The Netherlands.
- 2
Present address: Shell U.K., Exploration and Production, Aberdeen. Scotland.