Sticklepath lustleigh fault
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 … 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 variously as the Sticklepath Fault, Sticklepath Fault Zone, Lustleigh-Sticklepath Fault or Sticklepath-Lustleigh Fault.[1]
Sticklepath lustleigh fault
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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): … WebWe 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 ...
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... 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.
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 ... 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, …
WebDextral strike-slip movement on the Sticklepath-Lustleigh fault zone (SLFZ) is indicated by displacements of ?Permian and older rocks. Previous authors have inferred that the main …
WebOct 13, 2024 · Devon has a naturally occurring dissecting line called the Sticklepath - Lustleigh Fault Zone referred to in some text as Devon’s own San Andreas fault line. Running from North-West to South-East from near Clovelly in North Devon, it passes through the Dartmoor village of Sticklepath near Okehampton before ending in Torquay in South Devon. business law and strategy melvinWebThe 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 … handyman services sherwood parkWebA 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. business law and litigationWebDec 20, 1998 · For example, up to 10 km dextral strike-slip displacement has been suggested along the Sticklepath–Lustleigh fault zone ( Fig. 3 a) during the later stages of the Variscan Orogeny ( Holloway and Chadwick, 1986 ). business law assignmenthttp://ussher.org.uk/wp-content/uploads/journal/2005/14-Prudden.pdf business law associates llchttp://www.clayheritage.org/introduction-to-the-ball-clays-of-devon-and-dorset/how-the-ball-clay-deposits-occurred business law arlington heightsWebJan 6, 2024 · Enhanced Geothermal System (EGS) resources are an increasingly viable geothermal energy target and are at the frontier of novel renewable energy sources. They … business law articles 2018