Sunday, March 6, 2011

dykes and sills

Dykes and sills (Avencas Beach , Parede)

Dykes and sills (Avencas Beach , Parede)

The Whin Sill (top left image) in N. England provided a defensive cliff-line

The Whin Sill (top left image) in N. England provided a defensive cliff-line

However, the dyke–sill transition at Arraial do Cabo is not easily explained

However, the dyke–sill transition at Arraial do Cabo is not easily explained

 dykes and sills. In the same area, the casts of several ammonites are to

dykes and sills. In the same area, the casts of several ammonites are to

 to be of injected (dykes and sills) rather than depositional origin.

to be of injected (dykes and sills) rather than depositional origin.

 demonstrate classic examples of composite (acid-basic) dykes and sills.

demonstrate classic examples of composite (acid-basic) dykes and sills.

Hot liquid rock (magma) moved through the country rock and cooled solid to from these sills and dykes which together are called minor intrusions.

Hot liquid rock (magma) moved through the country rock and cooled solid to from these sills and dykes which together are called minor intrusions.

Dykes and sills of basic to ultrabasic composition of Mesozoic ages

Dykes and sills of basic to ultrabasic composition of Mesozoic ages

 lava flows, sills and dykes by ponding and contraction during cooling.

lava flows, sills and dykes by ponding and contraction during cooling.

This whole area is criss crossed with dykes and sills.

This whole area is criss crossed with dykes and sills.

Another diagram of how the dolerite sill and dykes were formed.

Another diagram of how the dolerite sill and dykes were formed.

GCPZC9 Dykes and Sills Earthcache - DP/EC2 (Earthcache) in Lisboa,

GCPZC9 Dykes and Sills Earthcache - DP/EC2 (Earthcache) in Lisboa,

 and form dykes/sills close to the Transition Zone Gabbro (TZG) horizon.

and form dykes/sills close to the Transition Zone Gabbro (TZG) horizon.

(2004). b) Trace element concentrations in mafic lavas, dykes and sills in

(2004). b) Trace element concentrations in mafic lavas, dykes and sills in

These rocks include volcanic rocks, igneous rocks of dykes and sills and

These rocks include volcanic rocks, igneous rocks of dykes and sills and

 mafic-intermediate intrusions (dykes and sills) and intermediate-felsic

mafic-intermediate intrusions (dykes and sills) and intermediate-felsic

 rock structure take place at the dyke–sill transition level (Fig. 3, 4).

rock structure take place at the dyke–sill transition level (Fig. 3, 4).

Felsic to intermediate porphyry dykes and sills occur in the Armina

Felsic to intermediate porphyry dykes and sills occur in the Armina

Small intrusions (dykes and sills) cool more quickly than large intrusions,

Small intrusions (dykes and sills) cool more quickly than large intrusions,

 criss crossed with dykes and sills - some of the best places to see

criss crossed with dykes and sills - some of the best places to see

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