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67 Ma, 15 to 9 Ma) and blocky calcites (30 Ma and 19 Ma), with MSWD (mean squared weighted deviates) between 0.20 and 18.

Different numerical ages were obtained from hydrothermal saddle dolomites (ca.Then enter the ‘name’ part of your Kindle email address below. Note you can select to send to either the @free.or @variations.‘’ emails are free but can only be sent to your device when it is connected to wi-fi.C dating of fossil bone with seriously depleted protein levels, or bone that has been consolidated with preservatives, can produce erroneous results.In the tropics, warm and moist soil conditions lead to constant reworking of organic matter and add to the danger of bone contamination.The steps needed to purify the samples are described, together with details on the use of qualitative infra-red (IR) spectra as a means of assessing sample purity.

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The very similar common lead composition (Pb) in solid bitumen and host limestone suggests Bekhme Formation tend to be synchronous with influx of hydrocarbon movement.

Consequently, the development of the Late Cretaceous folding and faulting phases and their reactivation during the Tertiary in the modeled area provided conduits for the HT fluids and hydrocarbon migrations along deeply seated faults.

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, (1)Department of Earth & Environmental Sciences, Université libre de Bruxelles (ULB), 50, avenue Franklin Roosevelt, Brussels, 1050, Belgium, (2)Department of Petroleum Geosciences, Soran University, Kawa Street, Soran-Kurdistan Region, 44008, Iraq, (3)Scientific Research Center, Soran University, Kawa Street, Soran-Kurdistan Region, 44008, Iraq, (4)Department of Earth and Atmospheric Sciences, Alberta University, Edmonton, AB T6G 2E3, Canada, (5)Institut für Geowissenschaften, Goethe Universität, Altenhöferallee 1, Frankfurt am Main, D-60438, Germany, (6)Geodynamics and Geofluids Research Grou, Departement of Earth and Environmental Sciences, KU Leuven, Celestijnenlaan 200E, Leuven, B-3001, Belgium, [email protected] The absolute ages of diagenetic carbonate phases are a vital parameter for the reconstruction of basin development and tectonic models.