--> ABSTRACT: Constraints on Thermal Evolution of Sedimentary Basins from Apatite Fission-Track Analysis, by P. F. Green, I. R. Duddy, A. J. W. Gleadow, K. A. Megarty, and J. F. Lovering; #91043 (2011)
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Constraints on Thermal Evolution of Sedimentary Basins from Previous HitApatiteNext Hit Previous HitFissionNext Hit-Previous HitTrackNext Hit Previous HitAnalysisNext Hit

P. F. Green, I. R. Duddy, A. J. W. Gleadow, K. A. Megarty, J. F. Lovering

Spontaneous Previous HitfissionNext Hit tracks in Previous HitapatiteNext Hit can reveal rigorous quantitative information on the thermal evolution of sedimentary basins in the temperature range of interest to the oil exploration industry. Over geologic time scales, Previous HitfissionNext Hit tracks in Previous HitapatiteNext Hit show readily measurable annealing effects in the temperature range of 20°-125°C, where the peak generation of liquid hydrocarbons also occurs.

Five Previous HitfissionNext Hit-Previous HittrackNext Hit parameters have been identified that are sensitive indicators of temperature. These parameters are the mean confined Previous HittrackNext Hit length, the distribution of confined Previous HittrackNext Hit lengths, the Previous HitfissionNext Hit Previous HittrackNext Hit age, the distribution of single grain ages, and the dependence of Previous HitfissionNext Hit-Previous HittrackNext Hit age with depth in borehole sequences.

The response of tracks to elevated temperature takes the form of a progressive shortening of individual tracks. This process is increasingly understood through detailed laboratory annealing experiments. The degree of shortening undergone by a single Previous HittrackNext Hit depends primarily on the maximum temperature to which the Previous HittrackNext Hit is exposed, with time being of only minor importance. This behavior, coupled with the continuous production of tracks through time, means that the final distribution of Previous HittrackNext Hit lengths directly reflects the thermal history. Since the Previous HitfissionNext Hit-Previous HittrackNext Hit age is a reflection of the distribution of Previous HittrackNext Hit lengths, the age also reflects the thermal history.

A quantitative understanding of these processes can be used to predict the Previous HitfissionNext Hit-Previous HittrackNext Hit parameters resulting from a postulated thermal history. Comparing such predictions with observed parameters allows rigorous constraints to be placed on viable thermal histories.

Previous HitApatiteNext Hit Previous HitfissionNext Hit-Previous HittrackNext Hit Previous HitanalysisNext Hit offers significant advantages over other techniques in the presence of only a single reaction pathway, insensitivity to environmental factors other than temperature, clear distinction between reworked and primary material, and the potential for rigorous quantitative Previous HitanalysisTop.

AAPG Search and Discovery Article #91043©1986 AAPG Annual Convention, Atlanta, Georgia, June 15-18, 1986.