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The outer parts of collision mountain belts are commonly represented by fold and thrust belts. Major advances in understanding these tectonic settings have aris
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Onshore fold-thrust belts are commonly perceived as 'difficult' places to explore for hydrocarbons and are therefore often avoided. However, these belts host la
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Orogenic belts and their shallow-soled fringes, the fold-thrust belts, are globally distributed in up to 20,000 km long mountain chains along the edges of the c
