Výsledky vyhledávání

Influence of extensional faults and relay ramp on palaeo‐topography and lacustrine carbonate facies: Purbeck Limestone Group (Upper Jurassic – Lower Cretaceous), Wessex Basin, UK

Autor: Peter M. Burgess, Dan Bosence, Arnaud Gallois

Publikováno v: Basin Research. 33:3159-3182

[Abstract Lacustrine carbonate facies distribution is controlled by multiple environmental parameters including climate, hydrology, and tectonic setting, but few published models address this complexity. In this study, seismic and borehole data, inte

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::3142ccf8672f78c1f88ba5b4e197d7d2
https://doi.org/10.1111/bre.12598

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Lacustrine carbonate platforms: Facies, cycles, and tectonosedimentary models for the presalt Lagoa Feia Group (Lower Cretaceous), Campos Basin, Brazil

Autor: M. C. Muniz, Dan Bosence

Publikováno v: AAPG Bulletin. 102:2569-2597

Studies of lacustrine carbonate rocks in continental rifts have received huge interest in recent years because of their great economic value in the South Atlantic. However, most existing facies and tectonosedimentary models for carbonate platforms ar

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::4ec5b6226e24e1b32e9d33138a6eec99
https://doi.org/10.1306/0511181620617087

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Discovery of enigmatic toroidal carbonate concretions on the Rio Grande Rise (Southwestern Atlantic Ocean)

Autor: Renata Moura de Mello, Matheus H. Vieira do Nascimento e Silva, Dan Bosence, Paulo César Fonseca Giannini, Paul Lusty, Mariana Benites, Christian Millo, Bramley J. Murton, Luigi Jovane, Paulo César Boggiani, R. Mark Leckie

Publikováno v: Repositório Institucional da USP (Biblioteca Digital da Produção Intelectual)
Universidade de São Paulo (USP)
instacron:USP

We present enigmatic toroidal carbonate concretions retrieved from 700 m water depth from two sites in the upper plateau of the Rio Grande Rise. The concretions have a diameter of ~15 cm and a central hole of ~5 cm, and were observed on top of loose

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d58d2f1dcee854ac7848441cb5466d08
https://doi.org/10.1016/j.margeo.2021.106665

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Discriminating between the origins of remotely sensed circular structures: carbonate mounds, diapirs or periclinal folds? Purbeck Limestone Group, Weymouth Bay, UK

Autor: Ian M. Watkinson, Arnaud Gallois, Jenny S. Collier, Dan Bosence, Simon Fleckner

Many sedimentary rock successions contain plan-view circular structures, such as impacts, diapirs and carbonate build-ups. When remotely sensed, it can be difficult to discriminate between their formation mechanisms. Here we examine this problem by a

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a11caeb56e2ee67e29866c1938f2374d
http://hdl.handle.net/10044/1/64930

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Brackish to hypersaline facies in lacustrine carbonates: Purbeck Limestone Group, Upper Jurassic-Lower Cretaceous, Wessex Basin, Dorset, UK

Autor: Dan Bosence, Peter M. Burgess, Arnaud Gallois

Publikováno v: FACIES

Sedimentary facies and stratigraphic architecture of non-marine carbonates are controlled by a range of environmental parameters, such as climate, hydrology and tectonic setting, but the few published facies models do not account for this variability

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a14309d9c5595b39bb9f0f61d7ce66b9
http://livrepository.liverpool.ac.uk/3019841/1/Gallois_et_al-2018-Facies.pdf

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Microbial carbonates in space and time: introduction

Autor: Bernard A. Vining, Tim Pritchard, Daniel Paul Le Heron, Dan Bosence, Kathryn Gibbons, William A. Morgan

Publikováno v: Geological Society, London, Special Publications. 418:1-15

DAN BOSENCE1*, KATHRYN GIBBONS2, DANIEL P. LE HERON1, WILLIAM A. MORGAN3, TIM PRITCHARD4 & BERNARD A. VINING1,5 Department Earth Sciences, Royal Holloway University of London, Egham, Surrey, TW20 0EX, UK Nexen Petroleum UK Ltd., Prospect House, 97 Ox

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::f5f5971fbae4382be49767ddefc5dfb1
https://doi.org/10.1144/sp418.14

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