Mineralogical, Morphological, Geochemical, and Chemical Studies of Guvenc Formation Shales, Adana Basin, South of Turkey: The Implication for Hydrocarbon Formation

被引:1
作者
Buyukutku, A. [1 ]
Gecer, A. [2 ]
机构
[1] Ankara Univ, Dept Geol Engn, Fac Engn, TR-06100 Ankara, Turkey
[2] Ankara Univ, Dept Chem Engn, Fac Engn, TR-06100 Ankara, Turkey
关键词
aromatic; geochemical; mineralogical; organic; pyrolysis; type III kerogen; DELTA;
D O I
10.1080/15567036.2012.684738
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
The mineralogical, morphological, chemical structure, and source of kerogen in the Guvenc shales were investigated. The X-ray diffraction patterns of bulk rock of all specimens indicated that they are mainly composed of chlorite, illite, smectite, quartz, calcite, feldspar, and dolomite minerals. Mixed layer smectite-chlorite and smectite-illite, and shell organism were determined according to scanning electron microscope analyses. Organic matter of Guvenc shales, which is mainly composed of type Ill kerogen, exhibits a relatively high aromatic character according to pyrolitic and Fourier transform infrared spectroscopy analysis. Geochemical analyses indicate that organic matter has the potential for gas generation.
引用
收藏
页码:2328 / 2336
页数:9
相关论文
共 12 条
[1]  
Bertrand Ph., 1993, APPL PETROLEUM GEOCH, P279
[2]   Clay controls on reservoir properties in sandstone of Kuzgun formation and its relevance to hydrocarbon exploration, Adana basin, Southern Turkey [J].
Büyükutku, AG ;
Bagci, AS .
JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING, 2005, 47 (3-4) :123-135
[3]  
Büyükutku AG, 2006, J GEOL SOC INDIA, V68, P615
[4]  
Espitalie J., 1980, AAPG BULL, V64, P1
[5]  
Espitalie J., 1977, Proceedings of the 9th Annual Offshore Technology Conference, V3, P439, DOI [10.4043/2935-MS, DOI 10.4043/2935-MS]
[6]   Origin and formation pathways of kerogen-like organic matter in recent sediments off the Danube delta (northwestern Black Sea) [J].
Garcette-Lepecq, A ;
Derenne, S ;
Largeau, C ;
Bouloubassi, I ;
Saliot, A .
ORGANIC GEOCHEMISTRY, 2000, 31 (12) :1663-1683
[7]   A TECTONICALLY CONTROLLED ALLUVIAL-FAN WHICH DEVELOPED INTO A MARINE FAN-DELTA AT A COMPLEX TRIPLE JUNCTION - MIOCENE-GILDIRLI FORMATION OF THE ADANA BASIN, TURKEY [J].
GORUR, N .
SEDIMENTARY GEOLOGY, 1992, 81 (3-4) :243-252
[8]   PROVENANCE OF MIOCENE SUBMARINE FANS IN THE NORTHERN ADANA BASIN, SOUTHERN TURKEY - A TEST OF DISCRIMINANT FUNCTION-ANALYSIS [J].
GURBUZ, K ;
KELLING, G .
GEOLOGICAL JOURNAL, 1993, 28 (3-4) :277-293
[9]  
Kerey I. E., 1985, 6 EUR REG M SED SPAI, P217
[10]  
Yalcin N. M., 1987, TURK 7 PETR C ANK TU, P427