Mesozoic and Cenozoic deformation inferred from seismic stratigraphy in the southwestern intracontinental Palmyride fold-thrust belt, Syria
نویسندگان
چکیده
منابع مشابه
Summary of the geological evolution of Syria through geophysical interpretation: Implications for hydrocarbon exploration
Intracontinental deformation, caused by plate boundary processes, dominates the past and present tectonics of Syria (Figure 1). This deformation has created structures that form hydrocarbon traps in several different areas of the country. Current production from Syria is around 600 000 b/d and the country hosts ongoing exploratory efforts. Deformation within Syria can be conveniently divided in...
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Allochthonous masses are common structures in Zagros fold-thrust belt. They are generally considered as collapse structures formed by the influence of gravity and in rock units with competency contrast. However, large allochthonous masses mapped in Dowgonbadan area in Dezful Embayment near the Mountain Front Fault (MFF) of Zagros show characteristics different from the belt common collapse stru...
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ژورنال
عنوان ژورنال: Geological Society of America Bulletin
سال: 1992
ISSN: 0016-7606
DOI: 10.1130/0016-7606(1992)104<0704:macdif>2.3.co;2