Zastosowanie izotopów w badaniach diagenezy osadów
Abstract
STABLE ISOTOPES IN STUDIES OF DIAGENESIS OF CLASTIC DEPOSITS
Summary
Isotopic composition of diagenetic minerals and porewaters in clastic sedimentary rocks can be used as a tracer for diagenetical history of the sediments. The stable isotopes of hydrogen, carbon, oxygen, sulphur, strontium and neodymium provide information about paleotemperature and water/rock/organic matter interactions and porewater evolution during diagenesis.
Summary
Isotopic composition of diagenetic minerals and porewaters in clastic sedimentary rocks can be used as a tracer for diagenetical history of the sediments. The stable isotopes of hydrogen, carbon, oxygen, sulphur, strontium and neodymium provide information about paleotemperature and water/rock/organic matter interactions and porewater evolution during diagenesis.