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Phd by thesis

Richard Lathe
- 01 Apr 1988 - 
- Vol. 332, Iss: 6166, pp 676-676
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TLDR
In this paper, a sedimentological core and petrographic characterisation of samples from eleven boreholes from the Lower Carboniferous of Bowland Basin (Northwest England) is presented.
Abstract
Deposits of clastic carbonate-dominated (calciclastic) sedimentary slope systems in the rock record have been identified mostly as linearly-consistent carbonate apron deposits, even though most ancient clastic carbonate slope deposits fit the submarine fan systems better. Calciclastic submarine fans are consequently rarely described and are poorly understood. Subsequently, very little is known especially in mud-dominated calciclastic submarine fan systems. Presented in this study are a sedimentological core and petrographic characterisation of samples from eleven boreholes from the Lower Carboniferous of Bowland Basin (Northwest England) that reveals a >250 m thick calciturbidite complex deposited in a calciclastic submarine fan setting. Seven facies are recognised from core and thin section characterisation and are grouped into three carbonate turbidite sequences. They include: 1) Calciturbidites, comprising mostly of highto low-density, wavy-laminated bioclast-rich facies; 2) low-density densite mudstones which are characterised by planar laminated and unlaminated muddominated facies; and 3) Calcidebrites which are muddy or hyper-concentrated debrisflow deposits occurring as poorly-sorted, chaotic, mud-supported floatstones. These

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References
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Mesoscopic theory for fluctuating active nematics

TL;DR: In this paper, a mesoscopic theory for active nematics was derived, complete with effective multiplicative noise terms, using a combination of kinetic theory and Ito calculus approaches, and the stochastic partial differential equations were shown to be at the origin of anomalous number fluctuations and long-range correlations.
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Stably ergodic diffeomorphisms which are not partially hyperbolic

TL;DR: In this paper, stable ergodicity of non-partially hyperbolic robustly transitive diffeomorphisms constructed by Bonatti-Viana has been shown, and the uniqueness of SRB (Sinai-Ruelle-Bowen) measure for non-conservative C − 1 perturbations of such diffeomorphic systems is verified.
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Hydrodynamics near a chiral critical point

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