Tectonically dewatered slates in the Ludlovian of the Lake District, England-Reference-Cited by-同舟云学术

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Tectonically dewatered slates in the Ludlovian of the Lake District, England

Published:2007-04-30 Issue:1 Volume:8 Page:95-110
ISSN:0072-1050
Container-title:Geological Journal
language:en
Short-container-title:Geol. J.

Author:

Mca. Powell C.

Publisher

Wiley

Subject

Geology

Reference53 articles.

1. The origin of slaty cleavage. Evidence from Precambrian rocks in Colorado;Braddock;Bull. geol. Soc. Am.,1970

2. On the maintenance of anomalous fluid pressures: I. thick sedimentary sequences;Bredehoeft;Bull. geol. Soc. Am.,1968

3. Development of flow cleavage in the Martinsburg shale, Port Jervis South area (Northern New Jersey);Carson;Tectonophys.,1967

4. Origin of slaty cleavage in the Coeur d'Alene district, Idaho;Clark;Bull. geol. Soc. Am.,1970

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1. Slaty cleavage associated with sandstone dykes in the Harlech Dome, North Wales;Geological Journal;2007-04-30

2. Post-tectonic clastic dykes in the Dalradian of Scotland and Ireland: implications for delayed lithification and deformation of sediments;Geological Journal;2000

3. Chemical and volume changes during deformation and prograde metamorphism of sediments;Geological Society, London, Special Publications;1998

4. Turbidite to storm transition in a migrating foreland basin: the Kendal Group (Upper Silurian), northwest England;Geological Magazine;1994-03

5. Foreland basin development and tectonics on the northwest margin of eastern Avalonia;Geological Magazine;1993-09

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