Sticklepath lustleigh fault

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August undefined, 2024

WebThe Lustleigh Fault 295 echelon fractures runs from Padley Common to the Gas Works (west of Chagford) and beyond. Another crosses the ridge of Waye Down, about a mile … http://www.clayheritage.org/introduction-to-the-ball-clays-of-devon-and-dorset/how-the-ball-clay-deposits-occurred

Sticklepath - Wikipedia

WebThe Sticklepath-Lustleigh fault zone: Tertiary sinistral reactivation of a Variscan dextral strike-slip fault Holloway, S.; Chadwick, R. A. Abstract. Publication: Journal of the … WebThe largest of these faults, such as the Sticklepath–Lustleigh fault, do not appear to cause more than a few degrees of rotation from the general E–W strike of beds. Tens of degrees of rotation... refurbished p340

The Sticklepath-Lustleigh fault zone: Tertiary sinistral reactivation ...

WebMay 1, 2009 · The north-eastern area of Dartmoor is traversed by a series of straight valleys which follow fault lines. One fault-system, which crosses the granite from near Lustleigh north-westwards to Stickle-path, is described in detail, and its relationships to structures in a wider area are briefly discussed. Type Articles Information Web(b) The Sticklepath-Lustleigh Fault Throughout the granite area of Dartmoor there is according to Clement Reid (1912, 57) a strong tendency for the smaller valleys to follow a north- west or north-north-west direction. WebThe Sticklepath Fault provided an almost unique set of circumstances which allowed formation and maintenance of these ball clay pits: erosion of rocks into fresh or brackish … refurbished p30 pro

The Production and Properties of Devon Ball Clays

WebMar 28, 2011 · The Sticklepath fault runs NW to SE in direction, and is thought to start at near Bideford in the North, running across the NE corner of Dartmoor and through to … WebThe Bovey Basin is a low-lying, diamond-shaped area of about 72 square kilometres drained by the Rivers Bovey and Teign. It is situated on the Sticklepath-Lustleigh fault zone between Newton Abbot and Bovey Tracey and results from subsidence within this zone. The main basin is centred on Heathfield and, the much smaller Decoy Basin, on the ... refurbished p40 pro 5gWebThe Sticklepath-Lustleigh Fault Zone, a structure known to have experienced multiple displacements[4], will be used as a control. The student will build and interpret 3D structural models of the fault zones. Dr Peacock is an expert in the safe and effective use of drones for geological studies[10] and will supervise these refurbished p30 pro new edition

"WebDec 20, 1998 · The largest of these faults, such as the Sticklepath–Lustleigh fault, do not appear to cause more than a few degrees of rotation from the general E–W strike of beds. … " - Sticklepath lustleigh fault

Sticklepath lustleigh fault

What might a fault-hosted geothermal reservoir look like?

WebThe Sticklepath-Lustleigh fault zone: Tertiary sinistral reactivation of a Variscan dextral strike-slip fault: HOLLOWAY, S. et al. Journal of the Geological Society (2007), 143 (3): … WebDr. W. R. D earman said that the Sticklepath-Lustleigh fault was the most prominent structure in the area, and the continuity of this north-westerly fracture had been …

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WebMay 1, 2009 · The Lustleigh Fault in north-east Dartmoor. Geol. Mag. 94, 291 –6.CrossRef Google Scholar. ... The Sticklepath-Lustleigh fault zone: Tertiary sinistral reactivation of a Variscan dextral strike-slip fault. Journal of the Geological Society, … http://ussher.org.uk/wp-content/uploads/journal/2005/14-Prudden.pdf

WebApart from map-scale structures, identification of minor structures associated with major faults, such as slickensides observed within the near-surface parts of fault zones, horsetail splays,... WebThe Sticklepath-Lustleigh faults played a major part in the deposition and preservation of the Tertiary ball clays in Devon. Deposition and Derivation of the Ball Clays The climate in the lower Tertiary period, in what is today Southwest England, was sub-tropical.

WebSticklepath is a village set amid the beautiful Dartmoor countryside. Its name derives from the Saxon ‘staecle’, meaning ‘steep’, as it lies at the foot of a high mount. Sticklepath is … WebSticklepath is a village on Dartmoor, in the county of Devon, England. It gives its name to one of the most important geological faults in south-west England, thought to have originated during the Tertiary period and known …

WebA major fault zone known as the great Sticklepath-Lustleigh fault zone is located to the east of Lundy (Figure 1). A fault zone comprises a significant number of parallel faults within a defined band and usually associated with, as the Sticklepath-Lustleigh fault is, …

WebCretaceous has been documented and the Sticklepath-Lustleigh Fault Zone in Devon has developed mid-Cenozoic strike-slip basins. The purpose of this work is to combine remote-sensed and historical ... refurbished p4000WebThe Sticklepath-Lustleigh Fault zone and associated Tertiary pull-apart basins e.g. Bovey Basin (Edwards, 1976); Petrockstow Basin (Bristow et al., 1992) are important ... Parrett Valley Fault, 1 km west of Ham Hill, has a dextral displacement on the basis that the E-W Coker Fault appears to have been offset. Harvey and Stewart (1998) have ... refurbished p40 proWebWe present an alternative model for the history of the Sticklepath-Lustleigh fault zone, summarized below: 1 Late Variscan strike-slip movement, with a total displacement of up to 10 km, produced the SLFZ and offset dextrally an earlier Variscan thrust. 2. Extensional reactivation of this thrust led to rapid Permo-Triassic subsidence in the ... refurbished p4 computersWebThe Sticklepath-Lustleigh fault zone: Tertiary sinistral reactivation of a Variscan dextral strike-slip fault Journal of the Geological Society 10.1144/gsjgs.143.3.0447 refurbished p463http://www.clayheritage.org/aspects-of-the-ball-clay-industry/the-production-and-properties-of-devon-ball-clays refurbished p64WebThe northeastern part of the Dartmoor granite mass in southwest England is traversed by a series of northwest-southeast valleys following fault lines. The name Lustleigh fault is … refurbished p50sWebA strong aeromagnetic anomaly, with a maximum over the peridotite SW of Coverack, extends both offshore and to the NW, across the mapped contact of the Crousa gabbro and western peridotite, and over the Traboe cumulate complex. At ground level, this anomaly appears to be discontinuous. refurbished p65c1