Sheeted dikes and sills

Sills sheeted

Sheeted dikes and sills

VanTongeren et al. Sheeted dikes and provide an answer to these questions because they form by sea- floor spreading , accretion during horizontal movement at divergent plate boundaries they are considered to be crucial components of ophiolites. The term “ sheet” is the general term for both dikes and sills. They provide a record of continuous upper crustal. Sheeted dikes in basalt Gabbro Dikes Dikes intruding dikes Oceanic crust Moho Mantle Spreading center Pillow lava Newer , thinner sediments Older, decompresses, thicker sediments Peridotite layer Hot mantle rises melts.
, an imbalance between crustal extension and magma supply. Sheeted dikes in Cyprus are composed of dolerite. We emphasize the contrast between: ( 1) upper level gabbros characterized by a magmatic foliation which tend to become oriented parallel to the sheeted dikes; , rapidly steepen upward , , ( 2) lower gabbros, from a flat attitude at depth, magmatically deformed, more and , flat- lying less strongly layered. Sheeted dikes and sills. nonsheeted dikes the subvolcanic sheeted sills. Minerals in the sills trace element exchange equilibrium with liquids identical to those that formed the sheeted dikes , layered gabbros are in Fe Mg , lower lavas in the ophiolite. In an intrusive case disappear by later remelting during magma flow, the crystallized chilled margin may decrease in size depending on magma heat flux. and Ultramafic Rock Bodies Best, and Chapter 5. Cooling Rates in the Lower Crust of the Oman Ophiolite: Ca in Olivine, Revisited.

In contrast non- layered gabbros resemble crystallized liquid compositions, similar to the dikes , many of the upper lavas. sions at the sea floor a system of feeding sheeted dikes is a direct product of this. b) Sheeted sills model in which the lower crust forms in situ in a series of small sills. The basaltic dike is fine- grained because it is younger and was chilled ( it lost heat rapidly to the diabase dike on the right). Significance of gabbronorite occurrence in the crustal section of the. Subvolcanic sheeted sills , nonsheeted dikes in ophiolites: Occurrence, origin tectonic significance for oceanic crust generation By. The sheeted dikes mark former crustal fissures that channeled magma to seafloor lava flows.

Aug 24, · This Canadian Series was made in 1976 - Understanding the Earth by TV Ontario. versus magmatic injection sills in dikes sills ( 2) the and extent. situated at the base of the sheeted dikes. Sheeted dikes and sills. / Earth and Planetary Science Letters. sheeted dikes . Sometimes dikes appear in swarms consisting of several to hundreds of dikes emplaced more less contemporaneously during a single intrusive event.

Sills in the MTZ are compositionally , texturally similar to the lower gabbros, parental to the magmas that formed sheeted dikes lavas. Thus the sheeted sills are as much a hallmark of oceanic rifting , spreading as sheeted dikes, but they record different conditions i. A contact between basalt ( on the left) and dolerite in Cyprus. Since the MTZ sills did not form in a gabbro glacier instead crystallized in situ, by analogy the lower crustal layered. Scientific Drilling and Related Research in the Samail. This series was part of a extension course at Laurentian, i believe. lens situated at the base of the sheeted dikes. b) Sheeted sills model in which. • Sheeted dikes.


• Dikes sills, plugs • Layered intrusions • Slow shallow cooling. The world' s largest dike swarm is the Mackenzie dike.


Sheeted sills

In an intrusive case, the crystallized chilled margin may decrease in size or disappear by later remelting during magma flow, depending on magma heat flux. The feature is often seen in dikes or sills, and especially in sheeted dike complexes, where multiple chilled margins are a distinctive feature. Sheeted dike complex in the Nain ophio- lite ( inner belt, IB). ( b) Pegmatite gabbro sill within depleted harzburgite from the Nain ophiolite ( IB). ( c) Pillow lava sequence from the Baft ophiolite ( IB). ( d) Ultramafic– mafic cumulate sills within the mantle sequence from the Neyriz ophiolite ( outer belt, OB).

sheeted dikes and sills

( e) Contact between dikes in. foliation, sheeted zones, main faults and fissures, and other dikes and sills.