Magma flow in dyke swarms of the Karoo LIP: Implications for the mantle plume hypothesis
Abstract The~ 183 Ma old Karoo Large Igneous Province extends across southern Africa
and is related to magmatism in Antarctica (west Dronning Maud Land and Transantarctic …
and is related to magmatism in Antarctica (west Dronning Maud Land and Transantarctic …
Lateral magma flow in mafic sill complexes
C Magee, JD Muirhead, A Karvelas… - …, 2016 - pubs.geoscienceworld.org
The structure of upper crustal magma plumbing systems controls the distribution of
volcanism and influences tectonic processes. However, delineating the structure and …
volcanism and influences tectonic processes. However, delineating the structure and …
Is this magnetic fabric normal? A review and case studies in volcanic formations
P Rochette, C Aubourg, M Perrin - Tectonophysics, 1999 - Elsevier
When studying weakly anisotropic rocks non-standard relationships between magnetic and
expected petrofabric axes are sometimes observed, in particular the so-called inverse or …
expected petrofabric axes are sometimes observed, in particular the so-called inverse or …
Anisotropy of magnetic susceptibility of lava flows and dykes: a historical account
E Cañón-Tapia - Geological Society, London, Special …, 2004 - lyellcollection.org
The basic assumptions made in the interpretation of the anisotropy of magnetic susceptibility
(AMS) of lava flows, dykes and other tabular intrusive rocks have changed with time. This …
(AMS) of lava flows, dykes and other tabular intrusive rocks have changed with time. This …
Occurrence and dispersal of magmas in the Jurassic Ferrar large igneous province, Antarctica
DH Elliot, TH Fleming - Gondwana Research, 2004 - Elsevier
Tholeiitic rocks of the Ferrar Large Igneous Province (FLIP) occur in a linear belt from the
Theron Mountains to Horn Bluff in the Transantarctic Mountains and extend into …
Theron Mountains to Horn Bluff in the Transantarctic Mountains and extend into …
On the interpretation of normal and inverse magnetic fabric in dikes: Examples from the Eger Graben, NW Bohemian Massif
M Chadima, V Cajz, P Týcová - Tectonophysics, 2009 - Elsevier
Recent studies of igneous rocks indicate that the predominant occurrence of normal/inverse
fabric in dikes may either reflect the presence of multi-domain (MD)/single-domain (SD) …
fabric in dikes may either reflect the presence of multi-domain (MD)/single-domain (SD) …
How are saucer‐shaped sills emplaced? Constraints from the Golden Valley Sill, South Africa
Magmatic sill intrusions develop saucer‐like geometries in layered sedimentary basins
intruded by large volumes of magma. Saucer‐shaped sill emplacement models are based …
intruded by large volumes of magma. Saucer‐shaped sill emplacement models are based …
Overlap of Karoo and Ferrar magma types in KwaZulu-Natal, South Africa
A suite of mafic dykes from the Underberg region of southern KwaZulu-Natal (South Africa)
were intruded at∼ 178 Ma, coincident in age with the major Okavango Dyke Swarm of …
were intruded at∼ 178 Ma, coincident in age with the major Okavango Dyke Swarm of …
Magma transport pathways in large igneous provinces: lessons from combining field observations and seismic reflection data
Abstract Large Igneous Province (LIP) formation involves the generation, intrusion, and
extrusion of significant volumes (typically> 1 Mkm 3) of mainly mafic magma and is …
extrusion of significant volumes (typically> 1 Mkm 3) of mainly mafic magma and is …
Rock texture and magnetic lineation in dykes: a simple analytical model
JP Callot, X Guichet - Tectonophysics, 2003 - Elsevier
We develop two simple models for simulating the combination of magnetic sub-fabrics
related to magma flow in dykes. The basic assumptions are (i) the petrofabric is …
related to magma flow in dykes. The basic assumptions are (i) the petrofabric is …