The Rusey Breccia, 80m long and 2-3m thick, occurs in the footwall of the Rusey Thrust, beneath the launch point of a series of thrust ramps. The thrust is a major Variscan structure exposed in the Boscastle shales on the north Cornish coast. The breccia forms a series of size graded layers, fining towards each layer boundary. The aligned clasts are surrounded in three dimensions by radial euhedral quartz. No fault gouge is present. The layering and re-brecciated clasts indicate repeated episodes of organisation and mineralisation. Clast organisation occurred in a dynamic environment resulting from episodic fluid injection associated with fault slip events, causing fluidisation of the clasts along the injection pathways. Mineralisation text...
The Carmel Head Thrust Belt (CHTB) is a major tectonic feature that records a complex history of pol...
The Cwm Llwyd Outlier of Namurian Middle Shales in the central part of the Black Mountain escarpment...
In the frontal part of the Rhenohercynian foreland fold-and-thrust belt (High-Ardenne slate belt, Ei...
Cockade breccias are a type of fault fills in which individual clasts are completely surrounded by c...
The Suicide Ridge Barren Breccia Pipe (not, vert, similar1527 ± 4 Ma) is one of numerous breccia occ...
The Bude Formation which crops out along a coastal section in north Cornwall represents a folded tur...
Chaotic breccias and megabreccias – locally called gash breccias – hosted within the Pembroke Limest...
Cockade breccias are fault fills in which individual clasts are completely surrounded by concentric ...
Chaotic breccias and megabreccias – locally called gash breccias – hosted within the Pembroke Limest...
Breccias in the Rusey Fault (Cornwall, UK) and the Roamane Fault (Porgera gold deposit, Papua New G...
Fault-related breccias, in Carboniferous limestone, have been well documented in the footwall damage...
The British Tertiary Igneous Province (BTIP) contains several large ‘breccia’ outcrops, classically ...
Recent conflicts in the interpretation of the structure of north Cornwall has resulted in the need f...
Flamborough Head chalks are located at the termination of E-W and N-S trending fault systems along t...
The obliqu-reverse Dent Fault, northwest England, throws Carboniferous limestone units in the footwa...
The Carmel Head Thrust Belt (CHTB) is a major tectonic feature that records a complex history of pol...
The Cwm Llwyd Outlier of Namurian Middle Shales in the central part of the Black Mountain escarpment...
In the frontal part of the Rhenohercynian foreland fold-and-thrust belt (High-Ardenne slate belt, Ei...
Cockade breccias are a type of fault fills in which individual clasts are completely surrounded by c...
The Suicide Ridge Barren Breccia Pipe (not, vert, similar1527 ± 4 Ma) is one of numerous breccia occ...
The Bude Formation which crops out along a coastal section in north Cornwall represents a folded tur...
Chaotic breccias and megabreccias – locally called gash breccias – hosted within the Pembroke Limest...
Cockade breccias are fault fills in which individual clasts are completely surrounded by concentric ...
Chaotic breccias and megabreccias – locally called gash breccias – hosted within the Pembroke Limest...
Breccias in the Rusey Fault (Cornwall, UK) and the Roamane Fault (Porgera gold deposit, Papua New G...
Fault-related breccias, in Carboniferous limestone, have been well documented in the footwall damage...
The British Tertiary Igneous Province (BTIP) contains several large ‘breccia’ outcrops, classically ...
Recent conflicts in the interpretation of the structure of north Cornwall has resulted in the need f...
Flamborough Head chalks are located at the termination of E-W and N-S trending fault systems along t...
The obliqu-reverse Dent Fault, northwest England, throws Carboniferous limestone units in the footwa...
The Carmel Head Thrust Belt (CHTB) is a major tectonic feature that records a complex history of pol...
The Cwm Llwyd Outlier of Namurian Middle Shales in the central part of the Black Mountain escarpment...
In the frontal part of the Rhenohercynian foreland fold-and-thrust belt (High-Ardenne slate belt, Ei...