Carbon-oxygen isotope analysis of fault rocks in carbonates from different orogenic cycles in the Cantabrian Zone (N Spain): similarities and differences
Abstract:<p>The isotopic carbon and oxygen isotope composition of carbonates (&#948;<sup>13</sup>C and &#948;<sup>18</sup>O), determined by temperature and the relative abundances of stable isotopes of both elements in water at the time the carbonate is precipitated, can be modified subsequently during geological processes that involve the recrystallization of carbonate. Temperature changes mostly affect &#948;<sup&… Show more
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