scholarly journals Geochemical summary log, TOC/rock-eval pyrolysis data, vitrinite reflectance data (410'-7930' only), and organic matter maturation values of cuttings (220'-11230') from the Alaska Consolidated Oil Iniskin Unit Zappa #1 well

1990 ◽  
Author(s):  
T. A. Edison
2021 ◽  
Author(s):  
Shahin Khosrov Akhundov ◽  
Mushfig Farhad Tagiyev ◽  
Arastun Ismail Khuduzade ◽  
Natig Namig Aliyev

Abstract Meso-Cenozoic sedimentary cover in the Middle Kura depression located between the Greater and Lesser Caucasus mountain structures contains numerous oil accumulations. According to studies in the Cretaceous and Paleogene strata, sedimentary organic matter is of mixed clastic-marine origin. Moderate amounts of organic matter have been recorded in the Eocene sediments (on average 0.70%), in the Upper and Lower Cretaceous average values made up 0.39% и 0.42%, respectively. Analysis of bitumoid composition suggests that in a number of areas bitumoids have experienced a widespread movement across the sedimentary strata. The results of measurements on isolated samples indicate that the Cretaceous strata have only advanced to the initial hard-coal stage of organic transformation (0.48-0.55%Ro). On vitrinite reflectance data the Eocene deposits in studied areas of the Middle Kura depression have reached initial (brown-coal) stage of catagenetic transformation (±0.48Ro%; est. paleotemperature of 85°C). Nonetheless, analysis of formation conditions of commercial HC accumulations found earlier in the Eocene strata allows considering them the most prospective in the Middle Kura depression.


Energies ◽  
2018 ◽  
Vol 11 (6) ◽  
pp. 1406 ◽  
Author(s):  
Seyedalireza Khatibi ◽  
Mehdi Ostadhassan ◽  
David Tuschel ◽  
Thomas Gentzis ◽  
Humberto Carvajal-Ortiz

Vitrinite maturity and programmed pyrolysis are conventional methods to evaluate organic matter (OM) regarding its thermal maturity. Moreover, vitrinite reflectance analysis can be difficult if prepared samples have no primary vitrinite or dispersed widely. Raman spectroscopy is a nondestructive method that has been used in the last decade for maturity evaluation of organic matter by detecting structural transformations, however, it might suffer from fluorescence background in low mature samples. In this study, four samples of different maturities from both shale formations of Bakken (the upper and lower members) Formation were collected and analyzed with Rock-Eval (RE) and Raman spectroscopy. In the next step, portions of the same samples were then used for the isolation of kerogen and analyzed by Raman spectroscopy. Results showed that Raman spectroscopy, by detecting structural information of OM, could reflect thermal maturity parameters that were derived from programmed pyrolysis. Moreover, isolating kerogen will reduce the background noise (fluorescence) in the samples dramatically and yield a better spectrum. The study showed that thermal properties of OM could be precisely reflected in Raman signals.


1994 ◽  
Vol 34 (1) ◽  
pp. 216 ◽  
Author(s):  
M.V. Ellacott ◽  
N.J. Russell ◽  
R.W.T. Wilkins

'Fluorescence alteration of multiple macerals' (FAMM) is a multi-parameter microprobe technique developed by CSIRO to provide the petroleum industry with an objective method of estimating thermal maturity of organic matter in sedimentary rocks. The technique is closely related to vitrinite reflectance methods, although the identification of vitrinite is not necessary; FAMM is based on the fluorescence alteration characteristics of vitrinite, inertinite and liptinite macerals in a sample. It is a powerful tool for the identification of casings, reworked material and hydrogen-rich (perhydrous) vitrinite, and has the capacity to correct for the effects of vitrinite reflectance suppression.The technique has been tested on Cretaceous coals from the Latrobe Group in Volador-1, offshore Gippsland Basin, where the identification of vitrinite is unequivocal, and on dispersed organic matter (DOM) in various clastic lithologies from the Cretaceous Waarre and Eumeralla Formations intersected by Flaxmans-1 and Port Campbell-4, onshore Otway Basin, where the identification of vitrinite is difficult and subjective.For the Volador-1 sequence, the FAMM-derived vitrinite reflectance (equivalent reflectance) and the measured vitrinite reflectance (VR) are similar, although the VR data are more scattered about the VR-depth regression line. The variability in the vitrinite reflectance data is largely due to compositional variation in the vitrinite. This variation however does not affect the equivalent vitrinite reflectance data to the same degree.In the sections intersected by Flaxmans-1 and Port Campbell-4, FAMM data indicate that vitrinite reflectance suppression is responsible for the large deviations of the measured values from the VR—depth regression line. In some of these samples the suppression effect may be as much as 0.20 per cent absolute.The FAMM technique offers a valuable supplement to VR determinations, or even a valid alternative in many practical situations.


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