Palynofacies, paleoenvironment and thermal maturity of early Silurian shales in Saudi Arabia (Qusaiba Member of Qalibah Formation)

[1]  Sreepat Jain Chitinozoa , 2019, Fundamentals of Invertebrate Palaeontology.

[2]  S. Inan,et al.  Thermo-vaporization for decontaminating hydrocarbon source rocks , 2018 .

[3]  G. Clayton,et al.  Application of Palynomorph Darkness Index (PDI) to assess the thermal maturity of palynomorphs: A case study from North Africa , 2018 .

[4]  T. Gentzis,et al.  Modified RGB-based kerogen maturation index (KMI): Correlation and calibration with classical thermal maturity indices , 2017 .

[5]  R. Goodhue,et al.  Correlation of Palynomorph Darkness Index and vitrinite reflectance in a submature Carboniferous well section in northern Saudi Arabia , 2017 .

[6]  M. Vecoli,et al.  A punctuated Late Ordovician and early Silurian deglaciation and transgression: Evidence from the subsurface of northern Saudi Arabia , 2017 .

[7]  S. Inan,et al.  A Petroleum System and Basin Modeling Study of Northwest and East-Central Saudi Arabia: Effect of Burial History and Adjacent Rock Lithology on the Gas Potential of the Silurian Qusaiba Shales , 2017 .

[8]  Khaled R. Arouri,et al.  The Silurian Qusaiba Hot Shales of Saudi Arabia: An integrated assessment of thermal maturity , 2016 .

[9]  J. Zalasiewicz,et al.  Early Silurian (Llandovery) graptolite assemblages of Saudi Arabia: biozonation, palaeoenvironmental significance and biogeography , 2016 .

[10]  W. Makled,et al.  Digital quantification of the miospore coloration to assess the thermal maturity: Novel RGB-based measuring technique , 2015 .

[11]  R. Littke,et al.  Optical thermal maturity parameters and organic geochemical alteration at low grade diagenesis to anchimetamorphism: A review , 2015 .

[12]  J. Verniers,et al.  Late Ordovician–earliest Silurian chitinozoans from the Qusaiba-1 core hole (North Central Saudi Arabia) and their relation to the Hirnantian glaciation , 2015 .

[13]  F. Paris,et al.  Late Ordovician scolecodonts from the Qusaiba-1 core hole, central Saudi Arabia, and their paleogeographical affinities , 2015 .

[14]  A. Hérissé,et al.  Late Ordovician to early Silurian acritarchs from the Qusaiba-1 shallow core hole, central Saudi Arabia , 2015 .

[15]  C. Kendall,et al.  Petroleum Systems of the Tethyan Region , 2014 .

[16]  A. Butcher,et al.  The middle Rhuddanian (lower Silurian) ‘hot’ shale of North Africa and Arabia: an atypical hydrocarbon source rock , 2013 .

[17]  G. Meinhold,et al.  Did lingering ice sheets moderate anoxia in the Early Palaeozoic of Libya? , 2013, Journal of the Geological Society.

[18]  C. Vasconcelos,et al.  Amorphous organic matter — Experimental data on formation and the role of microbes , 2011 .

[19]  J. Moreau The Late Ordovician deglaciation sequence of the SW Murzuq Basin (Libya) , 2011 .

[20]  R. Goodhue,et al.  Palynomorph Darkness Index (PDI) — A New Technique for Assessing Thermal Maturity , 2010 .

[21]  J. Zalasiewicz,et al.  Graptolites in British stratigraphy , 2009, Geological Magazine.

[22]  G. Clayton,et al.  Colour change in the acritarch Veryhachium as an indicator of thermal maturity , 2008, GeoArabia.

[23]  Mark Williams,et al.  Origin, sequence stratigraphy and depositional environment of an upper Ordovician (Hirnantian) deglacial black shale, Jordan , 2006 .

[24]  S. Lüning,et al.  Anatomy of a world-class source rock: Distribution and depositional model of Silurian organic-rich shales in Jordan and implications for hydrocarbon potential , 2005 .

[25]  R. Littke,et al.  Paleozoic petroleum systems of Saudi Arabia: a basin modeling approach , 2005, GeoArabia.

[26]  A. Merrell,et al.  Significant new biostratigraphic horizons in the Qusaiba Member of the Silurian Qalibah Formation of central Saudi Arabia, and their sedimentologic expression in a sequence stratigraphic context , 2005, GeoArabia.

[27]  M. Vecoli Palaeoenvironmental interpretation of microphytoplankton diversity trends in the Cambrian–Ordovician of the northern Sahara Platform , 2000 .

[28]  S. Lüning,et al.  Lower Silurian `hot shales' in North Africa and Arabia: regional distribution and depositional model , 2000 .

[29]  J. Marshall,et al.  Spore transmittance (% St): a quantitative method for spore colour analysis , 1999 .

[30]  S. Williams,et al.  Thermal maturity and burial history of Paleozoic rocks in western Newfoundland , 1998 .

[31]  J. Marshall,et al.  Quantitative spore colour measurement using colour image analysis , 1998 .

[32]  L. E. Wender,et al.  Paleozoic (Pre-Khuff Hydrocarbon Geology of the Ghawar Area, Eastern Saudi Arabia , 1998, GeoArabia.

[33]  R. Wicander,et al.  The use of microphytoplankton and chitinozoans for interpreting transgressive/regressive cycles in the Rapid Member of the Cedar Valley Formation (Middle Devonian), Iowa , 1997 .

[34]  R. Tyson Sedimentary Organic Matter , 1995 .

[35]  G. A. Cole Graptolite-Chitinozoan Reflectance and Its Relationship to Other Geochemical Maturity Indicators in the Silurian Qusaiba Shale, Saudi Arabia , 1994 .

[36]  J. Marshall Quantitative spore colour , 1991, Journal of the Geological Society.

[37]  Tx,et al.  Transmittance Color Index (TCI) of Amorphous Organic Matter: New Thermal Maturity Indicator for Hydrocarbon Source Rocks, Correlation with Mean Vitrinite Reflectance and Thermal Alteration Index (TAI): ABSTRACT , 1989 .

[38]  D. Welte,et al.  Petroleum Formation and Occurrence , 1989 .

[39]  F. Goodarzi,et al.  Graptolite reflectance and thermal maturity of Lower and Middle Ordovician shales from Scania, Sweden , 1988 .

[40]  R. Tyson The genesis and palynofacies characteristics of marine petroleum source rocks , 1987, Geological Society, London, Special Publications.

[41]  Kenneth E. Peters,et al.  Guidelines for Evaluating Petroleum Source Rock Using Programmed Pyrolysis , 1986 .

[42]  D. Batten,et al.  Maturation of organic matter in Cretaceous strata of the Northern Calcareous Alps , 1985 .

[43]  D. Batten Identification of Amorphous Sedimentary Organic Matter by Transmitted Light Microscopy , 1983, Geological Society, London, Special Publications.

[44]  P. Smith Spectral Correlation of Spore Coloration Standards , 1983, Geological Society, London, Special Publications.

[45]  D. Batten Palynofacies, palaeoenvironments and petroleum , 1982, Journal of Micropalaeontology.

[46]  C. Barnes,et al.  Thermal maturation, burial history and hotspot development, Paleozoic strata of southern Ontario-Quebec, from conodont acritarch colour alteration studies , 1981 .

[47]  K. Dorning Silurian acritarchs from the type Wenlock and Ludlow of Shropshire, England , 1981 .

[48]  L. D. Harris,et al.  Conodont color alteration; an index to organic metamorphism , 1975 .

[49]  M. Correia DIAGENESIS OF SPOROPOLLENIN AND OTHER COMPARABLE ORGANIC SUBSTANCES: APPLICATION TO HYDROCARBON RESEARCH , 1971 .

[50]  Frank L. Staplin,et al.  SEDIMENTARY ORGANIC MATTER, ORGANIC METAMORPHISM, AND OIL AND GAS OCCURRENCE , 1969 .