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| | [No title] (Site not responding. Last check: 2007-10-11) |
 | | In Portugal, these include: (1) the Iberian terrane, which occupies most of the Massif, shows Gondwanian affinities at least until the late Proterozoic and is considered the Iberian autochthon (it includes the Central Iberian and Ossa-Morena zones, cf. |
 | | The latter is essentially a metasedimentary unit with minor representation of ophiolite melanges and volcanic rocks with a typical N-MORB chemistry (from the base upwards: serpentinites, flaser gabbros, massive and banded gabbros, sheeted dikes, and pillow basalts) (Quesada et al., 1994; Ribeiro and Silva, in press). |
 | | The Iberian terrane (which includes the Central Iberian Zone and the Ossa Morena Zone) seems to extend from northernmost Iberia to south of the Nazaré canyon. |
| www.ga.gov.au /odp/publications/149_SR/chap_01/c1_5.htm (1692 words) |
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