The Ollo de Sapo Formation comprises variably metamorphosed felsic peraluminous volcanic rocks and highlevel granites that crop out over some 600km from the Cantabrian coast to central Spain in the northern part of the Central Iberian Zone.
P. MONTERO, C. TALAVERA, F. BEA
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Microcontinent subduction and S-type volcanism prior to India-Asia collision. [PDF]
Yang Z +7 more
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Long-term preservation of Hadean protocrust in Earth's mantle. [PDF]
Tusch J +6 more
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Transmogrification of ocean into continent: implications for continental evolution. [PDF]
Morgan JP, Vannucchi P.
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Petrogenesis and tectonic significance of the Baipu granite porphyry in the Huangtian uranium deposit, northeastern Guangdong, South China. [PDF]
Ruan K, Wu J, Long Z, Min Z.
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Contrasting volcano spacing along SW Japan arc caused by difference in age of subducting lithosphere. [PDF]
Tatsumi Y +4 more
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Passive margins in accreting Archaean archipelagos signal continental stability promoting early atmospheric oxygen rise. [PDF]
Peng Y +7 more
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Percolative sulfide core formation in oxidized planetary bodies. [PDF]
Crossley SD +9 more
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High-enthalpy Larderello geothermal system, Italy, powered by thousands of cubic kilometres of mid-crustal magma. [PDF]
Lupi M +17 more
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