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The geology of the Iberian Peninsula consists of the study of the rock formations on the Iberian Peninsula, which includes Spain, Portugal, Andorra, and Gibraltar. The peninsula contains rocks from every age from Ediacaran to Holocene, and almost every kind of rock is represented. World class mineral deposits can also be found there. The core of the Iberian Peninsula consists of a Hercynian cratonic block known as the Iberian Massif. On the northeast this is bounded by The Pyrenean fold belt, and on the southeast it is bounded by the Betic Foldchain. These twofold chains are part of the Alpine belt. To the west, the peninsula is delimited by the continental boundary formed by the opening of the Atlantic Ocean. The Hercynian Foldbelt is mostly buried by Mesozoic and Cenozoic cover rocks to the east, but nevertheless outcrops through the Iberian Chain and the Catalonian Coastal Ranges. ==Iberian Massif== The Iberian Massif consists of rocks from the Paleozoic Era. It was assembled about 310 Ma. Several zones occur in the Iberian Massif. These were the pieces that were assembled to form the block. On the north coast of Spain occurs the Cantabrian Zone. Then to the west and also in the Iberian Chain and Catalonian Coastal Ranges is the West Asturian-Leonese Zone. Then the Central Iberian Zone appears near A Coruña, through the north of Portugal, and through the middle of Spain, including the Montes de Toledo. The Ossa-Morena Zone outcrops out to the east of Lisbon. This includes some Precambrian rocks. The furthest south part is the South-Portuguese Zone. The Variscan Orogeny occurred as the European Hunic Terrane (split off from Gondwana) and Laurentia-Baltica continents collided. In Iberia this occurred in pre-Stephanian Carboniferous (354–305 Ma). The external part of the orogeny was the Cantabrian Zone. This was deformed in the upper crustal layers. The West Asturian Leonese Zone and Central Iberian Zone are the external parts of the orogeny and are more deeply deformed and metamorphosed, and intruded. These three zones are part of one terrane. The Ossa-Morena Zone and South Portuguese Zone are two different terranes that have become attached. In the Mesozoic this was mostly covered with other sediments, which have since eroded. 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Geology of the Iberian Peninsula」の詳細全文を読む スポンサード リンク
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