Abstract
The research reconsidered the sequences of the Late Cretaceous stratigraphic column represented by the formations of (Ahmadi, Rumaila, Mishrif/Kafl, Khasib, Tanuma, Saadi, Hartha, Shiransh and Tiyarat) in southern Iraq, through the study of nine oil wells distributed in nine oil fields, which are (Ghulaisan, Diwan, Arfidain, Amara, Halfaya, Abu Khaima, Rumaila al-Shamali, West Qurna, and Majnoun), where the research relied on the principles of stratigraphic sequences in the analysis The stratigraphic analysis was used to provide a clearer and more comprehensive picture of the formations of the research area. The Late Cretaceous sequences were characterized by deep basinal calcareous facies in general with cases of relative shallowing that were mainly caused by the factor of global sea level change. The research also tried to provide a clear picture of the change in the absorption space during the Late Cretaceous period by relying on the cycles of base level changes that proved the existence of four cycles. Half a cycle of the third degree in the southern and southwestern parts and only four cycles in the northern and northeastern parts of the study area. This was clarified by means of the two comparison sections, where the distinctive stratigraphic surfaces were identified, the most important of which were the maximum flood surfaces, and their number was five maximum flood surfaces that contained four inherent stratigraphic sequences. The research concluded by dividing the paths of the systems as a general view as follows: The Ahmadi Formation and the Rumaila Formation represent the path of the inundation system, while the Mishrif Formation represents the path of the high system, while the Kafel Formation, which is equivalent to it, represents the path of the low system, and the Khasib Formation represents the path of the inundation system, while the Tanuma Formation and the lower part of the Saadi Formation represent the path of the high system, while the upper part of the Saadi Formation is within the path of the system. The submerged formation represents the Hartha Formation of the upper system path, and the Shirnish Formation is within the submerged system path, while the final formation of the upper Cretaceous is the Tayarat Formation, which represents the upper system path. The kinetic activity of the compressional phase type in the Late Cretaceous period had a great impact on drawing the physiographical features of the sedimentary basin, and its impact was evident in the disappearance of the Tayarat Formation in some of the study wells, especially in the wells of eastern Maysan.
Abstract
اﻋﺎد اﻟﺒﺤث اﻟﻨظر ﻓﻲ ﺘﺘﺎﺒﻌﺎت اﻟﻌﻤود اﻟطﺒﺎﻗﻲ ﻟﻠﻌﺼر اﻟطﺒﺎﺸﻴري اﻟﻤﺘﺄﺨ ارﻟﻤﺘﻤﺜﻝ ﺒﺘﻛوﻴﻨﺎت )اﺤﻤدي و رﻤﻴﻠﺔ و ﻤﺸرف/ ﻛﻔﻝ و ﺨﺼﻴب و ﺘﻨوﻤﺔ و ﺴﻌدي و ﻫﺎرﺜﺔ و ﺸﻴ ارﻨش و طﻴﺎ ارت ( ﺠﻨوب اﻟﻌ ارق ،ﻤن ﺨﻼﻝ د ارﺴﺔ ﺘﺴﻌﺔ اﺒﺎر
ﻨﻔطﻴﺔ ﻤوزﻋﺔ ﻓﻲ ﺘﺴﻊ ﺤﻘوﻝ ﻨﻔطﻴﺔ ﻫﻲ ) ﻏﻠﻴﺼﺎن،و دﻴوان،و ارﻓدﻴن،و ﻋﻤﺎرة،وﺤﻠﻔﺎﻴﺔ، و اﺒو ﺨﻴﻤﺔ،و رﻤﻴﻠﺔ اﻟﺸﻤﺎﻟﻲ،و
ﻏرب اﻟﻘرﻨﺔ، و ﻤﺠﻨون (، ﺤﻴث اﻋﺘﻤد اﻟﺒﺤث ﻤﺒﺎدئ طﺒﺎﻗﻴﺔ اﻟﺘﺘﺎﺒﻌﺎت ﻓﻲ اﻟﺘﺤﻠﻴﻝ اﻟطﺒﺎﻗﻲ ﻻﻋطﺎء ﺼورة اوﻀﺢ واﺸﻤﻝ ﻟﺘﻛوﻴﻨﺎت ﻤﻨطﻘﺔ اﻟﺒﺤث. اﻤﺘﺎزت ﺘﺘﺎﺒﻌﺎت اﻟطﺒﺎﺸﻴري اﻟﻤﺘﺄﺨر ﺒﺎﻟﺴﺤﻨﺎت اﻟﺠﻴرﻴﺔ اﻟﺤوﻀﻴﺔ اﻟﻌﻤﻴﻘﺔ ﺒﺼورة ﻋﺎﻤﺔ ﻤﻊ ﺤﺎﻻت ﻤن اﻟﺘﻀﺤﻝ اﻟﻨﺴﺒﻲ اﻟذي ﻛﺎن ﺴﺒﺒﻪ ﻋﺎﻤﻝ ﺘﻐﺎﻴر ﻤﺴﺘوى ﺴطﺢ اﻟﺒﺤر اﻟﻌﺎﻟﻤﻲ ﺒﺸﻛﻝ اﺴﺎﺴﻲ ،ﻛﻤﺎ ﺤﺎوﻝ اﻟﺒﺤث اﻋطﺎء ﺼورة واﻀﺤﺔ ﻟﺘﻐﺎﻴر ﻓﻀﺎء اﻻﺴﺘﻴﻌﺎب ﺨﻼﻝ ﻓﺘرة اﻟطﺒﺎﺸﻴري اﻟﻤﺘﺄﺨر وذﻟك ﻋن طرﻴق اﻻﻋﺘﻤﺎد ﻋﻠﻰ دو ارت ﺘﻐﺎﻴ ارت ﻤﺴﺘوى اﻟﻘﺎﻋدة اﻟﺘﻲ اﺜﺒﺘت وﺠود ارﺒﻊ دو ارت وﻨﺼف دورة ﻤن اﻟدرﺠﺔ اﻟﺜﺎﻟﺜﺔ ﻓﻲ اﻻﺠ ازء اﻟﺠﻨوﺒﻴﺔ واﻟﺠﻨوﺒﻴﺔ اﻟﻐرﺒﻴﺔ وارﺒﻊ
دو ارت ﻓﻘط ﻓﻲ اﻻﺠ ازء اﻟﺸﻤﺎﻟﻴﺔ واﻟﺸﻤﺎﻟﻴﺔ اﻟﺸرﻗﻴﺔ ﻤن ﻤﻨطﻘﺔ اﻟد ارﺴﺔ. ﺘم ﺘوﻀﻴﺢ ذﻟك ﻋن طرﻴق ﻤﻘطﻌﻲ اﻟﻤﻀﺎﻫﺎة، اذ ﺘم ﺘﺤدﻴد اﻻﺴطﺢ اﻟطﺒﺎﻗﻴﺔ اﻟﻤﻤﻴزة اﻟﺘﻲ ﻤن اﻫﻤﻬﺎ ﺴطوح اﻟﻔﻴﻀﺎن اﻻﻗﺼﻰ وﻛﺎن ﻋددﻫﺎ ﺨﻤس اﺴطﺢ ﻓﻴﻀﺎن اﻗﺼﻰ اﺤﺘوت ارﺒﻊ ﺘﺘﺎﺒﻌﺎت طﺒﺎﻗﻴﺔ ﻤﺘﺄﺼﻠﺔ ﻤﻨﺸﺄﻴﺎ . ﺨﻠص اﻟﺒﺤث اﻟﻰ ﺘﻘﺴﻴم ﻤﺴﺎ ارت اﻻﻨظﻤﺔ ﻛﻨظرة ﻋﺎﻤﺔ ﻋﻠﻰ اﻟﻨﺤو اﻟﺘﺎﻟﻲ ﺘﻛوﻴن اﻻﺤﻤدي وﺘﻛوﻴن اﻟرﻤﻴﻠﺔ ﻴﻤﺜﻼن ﻤﺴﺎر اﻟﻨظﺎم اﻻﻏﻤﺎري اﻤﺎ ﺘﻛوﻴن اﻟﻤﺸرف ﻓﻬو ﻴﻤﺜﻝ ﻤﺴﺎر اﻟﻨظﺎم اﻟﻌﺎﻟﻲ ﺒﻴﻨﻤﺎ ﻴﻤﺜﻝ ﺘﻛوﻴن ﻛﻔﻝ اﻟذي ﻴﻛﺎﻓﺌﻪ ﻤﺴﺎر اﻟﻨظﺎم اﻟواطﻰء وﻴﻤﺜﻝ ﺘﻛوﻴن اﻟﺨﺼﻴب ﻤﺴﺎر اﻟﻨظﺎم اﻻﻏﻤﺎري اﻤﺎ ﺘﻛوﻴن ﺘﻨوﻤﺔ واﻟﺠزء اﻻﺴﻔﻝ ﻤن ﺘﻛوﻴن اﻟﺴﻌدي ﻓﻴﻤﺜﻝ ﻤﺴﺎر اﻟﻨظﺎم اﻟﻌﺎﻟﻲ ﺒﻴﻨﻤﺎ ﻴﻛون اﻟﺠزء اﻻﻋﻠﻰ ﻤن ﺘﻛوﻴن اﻟﺴﻌدي ﻀﻤن ﻤﺴﺎر اﻟﻨظﺎم اﻻﻏﻤﺎري وﻴﻤﺜﻝ ﺘﻛوﻴن ﻫﺎرﺜﺔ ﻤﺴﺎر اﻟﻨظﺎم اﻟﻌﺎﻟﻲ وﻴﻛون ﺘﻛوﻴن ﺸﻴ ارﻨش ﻀﻤن ﻤﺴﺎر اﻟﻨظﺎم اﻻﻏﻤﺎري اﻤﺎ ﺨﺎﺘﻤﺔ ﺘﻛوﻴﻨﺎت اﻟطﺒﺎﺸﻴري اﻻﻋﻠﻰ وﻫو ﺘﻛوﻴن طﻴﺎ ارت ﻴﻤﺜﻝ ﻤﺴﺎر اﻟﻨظﺎم اﻟﻌﺎﻟﻲ. ان اﻟﻨﺸﺎط اﻟﺤرﻛﻲ ﻤن ﻨوع اﻟطور اﻻﻨﻀﻐﺎطﻲ ﻓﻲ ﻓﺘرة اﻟطﺒﺎﺸﻴري اﻟﻤﺘﺄﺨر ﻛﺎن ﻟﻬﺎ اﻻﺜر اﻟﻛﺒﻴر ﻓﻲ رﺴم ﻓﻴزﻴوﻏ ارﻓﻴﺔ ﺤوض اﻟﺘرﺴﻴب واﺘﻀﺢ اﺜرﻫﺎ ﻓﻲ اﺨﺘﻔﺎء ﺘﻛوﻴن اﻟطﻴﺎ ارت ﻓﻲ ﺒﻌض اﺒﺎر
اﻟد ارﺴﺔ ﺨﺼوﺼﺎ ﻓﻲ اﺒﺎر ﺸرق ﻤﻴﺴﺎن .
ﻨﻔطﻴﺔ ﻤوزﻋﺔ ﻓﻲ ﺘﺴﻊ ﺤﻘوﻝ ﻨﻔطﻴﺔ ﻫﻲ ) ﻏﻠﻴﺼﺎن،و دﻴوان،و ارﻓدﻴن،و ﻋﻤﺎرة،وﺤﻠﻔﺎﻴﺔ، و اﺒو ﺨﻴﻤﺔ،و رﻤﻴﻠﺔ اﻟﺸﻤﺎﻟﻲ،و
ﻏرب اﻟﻘرﻨﺔ، و ﻤﺠﻨون (، ﺤﻴث اﻋﺘﻤد اﻟﺒﺤث ﻤﺒﺎدئ طﺒﺎﻗﻴﺔ اﻟﺘﺘﺎﺒﻌﺎت ﻓﻲ اﻟﺘﺤﻠﻴﻝ اﻟطﺒﺎﻗﻲ ﻻﻋطﺎء ﺼورة اوﻀﺢ واﺸﻤﻝ ﻟﺘﻛوﻴﻨﺎت ﻤﻨطﻘﺔ اﻟﺒﺤث. اﻤﺘﺎزت ﺘﺘﺎﺒﻌﺎت اﻟطﺒﺎﺸﻴري اﻟﻤﺘﺄﺨر ﺒﺎﻟﺴﺤﻨﺎت اﻟﺠﻴرﻴﺔ اﻟﺤوﻀﻴﺔ اﻟﻌﻤﻴﻘﺔ ﺒﺼورة ﻋﺎﻤﺔ ﻤﻊ ﺤﺎﻻت ﻤن اﻟﺘﻀﺤﻝ اﻟﻨﺴﺒﻲ اﻟذي ﻛﺎن ﺴﺒﺒﻪ ﻋﺎﻤﻝ ﺘﻐﺎﻴر ﻤﺴﺘوى ﺴطﺢ اﻟﺒﺤر اﻟﻌﺎﻟﻤﻲ ﺒﺸﻛﻝ اﺴﺎﺴﻲ ،ﻛﻤﺎ ﺤﺎوﻝ اﻟﺒﺤث اﻋطﺎء ﺼورة واﻀﺤﺔ ﻟﺘﻐﺎﻴر ﻓﻀﺎء اﻻﺴﺘﻴﻌﺎب ﺨﻼﻝ ﻓﺘرة اﻟطﺒﺎﺸﻴري اﻟﻤﺘﺄﺨر وذﻟك ﻋن طرﻴق اﻻﻋﺘﻤﺎد ﻋﻠﻰ دو ارت ﺘﻐﺎﻴ ارت ﻤﺴﺘوى اﻟﻘﺎﻋدة اﻟﺘﻲ اﺜﺒﺘت وﺠود ارﺒﻊ دو ارت وﻨﺼف دورة ﻤن اﻟدرﺠﺔ اﻟﺜﺎﻟﺜﺔ ﻓﻲ اﻻﺠ ازء اﻟﺠﻨوﺒﻴﺔ واﻟﺠﻨوﺒﻴﺔ اﻟﻐرﺒﻴﺔ وارﺒﻊ
دو ارت ﻓﻘط ﻓﻲ اﻻﺠ ازء اﻟﺸﻤﺎﻟﻴﺔ واﻟﺸﻤﺎﻟﻴﺔ اﻟﺸرﻗﻴﺔ ﻤن ﻤﻨطﻘﺔ اﻟد ارﺴﺔ. ﺘم ﺘوﻀﻴﺢ ذﻟك ﻋن طرﻴق ﻤﻘطﻌﻲ اﻟﻤﻀﺎﻫﺎة، اذ ﺘم ﺘﺤدﻴد اﻻﺴطﺢ اﻟطﺒﺎﻗﻴﺔ اﻟﻤﻤﻴزة اﻟﺘﻲ ﻤن اﻫﻤﻬﺎ ﺴطوح اﻟﻔﻴﻀﺎن اﻻﻗﺼﻰ وﻛﺎن ﻋددﻫﺎ ﺨﻤس اﺴطﺢ ﻓﻴﻀﺎن اﻗﺼﻰ اﺤﺘوت ارﺒﻊ ﺘﺘﺎﺒﻌﺎت طﺒﺎﻗﻴﺔ ﻤﺘﺄﺼﻠﺔ ﻤﻨﺸﺄﻴﺎ . ﺨﻠص اﻟﺒﺤث اﻟﻰ ﺘﻘﺴﻴم ﻤﺴﺎ ارت اﻻﻨظﻤﺔ ﻛﻨظرة ﻋﺎﻤﺔ ﻋﻠﻰ اﻟﻨﺤو اﻟﺘﺎﻟﻲ ﺘﻛوﻴن اﻻﺤﻤدي وﺘﻛوﻴن اﻟرﻤﻴﻠﺔ ﻴﻤﺜﻼن ﻤﺴﺎر اﻟﻨظﺎم اﻻﻏﻤﺎري اﻤﺎ ﺘﻛوﻴن اﻟﻤﺸرف ﻓﻬو ﻴﻤﺜﻝ ﻤﺴﺎر اﻟﻨظﺎم اﻟﻌﺎﻟﻲ ﺒﻴﻨﻤﺎ ﻴﻤﺜﻝ ﺘﻛوﻴن ﻛﻔﻝ اﻟذي ﻴﻛﺎﻓﺌﻪ ﻤﺴﺎر اﻟﻨظﺎم اﻟواطﻰء وﻴﻤﺜﻝ ﺘﻛوﻴن اﻟﺨﺼﻴب ﻤﺴﺎر اﻟﻨظﺎم اﻻﻏﻤﺎري اﻤﺎ ﺘﻛوﻴن ﺘﻨوﻤﺔ واﻟﺠزء اﻻﺴﻔﻝ ﻤن ﺘﻛوﻴن اﻟﺴﻌدي ﻓﻴﻤﺜﻝ ﻤﺴﺎر اﻟﻨظﺎم اﻟﻌﺎﻟﻲ ﺒﻴﻨﻤﺎ ﻴﻛون اﻟﺠزء اﻻﻋﻠﻰ ﻤن ﺘﻛوﻴن اﻟﺴﻌدي ﻀﻤن ﻤﺴﺎر اﻟﻨظﺎم اﻻﻏﻤﺎري وﻴﻤﺜﻝ ﺘﻛوﻴن ﻫﺎرﺜﺔ ﻤﺴﺎر اﻟﻨظﺎم اﻟﻌﺎﻟﻲ وﻴﻛون ﺘﻛوﻴن ﺸﻴ ارﻨش ﻀﻤن ﻤﺴﺎر اﻟﻨظﺎم اﻻﻏﻤﺎري اﻤﺎ ﺨﺎﺘﻤﺔ ﺘﻛوﻴﻨﺎت اﻟطﺒﺎﺸﻴري اﻻﻋﻠﻰ وﻫو ﺘﻛوﻴن طﻴﺎ ارت ﻴﻤﺜﻝ ﻤﺴﺎر اﻟﻨظﺎم اﻟﻌﺎﻟﻲ. ان اﻟﻨﺸﺎط اﻟﺤرﻛﻲ ﻤن ﻨوع اﻟطور اﻻﻨﻀﻐﺎطﻲ ﻓﻲ ﻓﺘرة اﻟطﺒﺎﺸﻴري اﻟﻤﺘﺄﺨر ﻛﺎن ﻟﻬﺎ اﻻﺜر اﻟﻛﺒﻴر ﻓﻲ رﺴم ﻓﻴزﻴوﻏ ارﻓﻴﺔ ﺤوض اﻟﺘرﺴﻴب واﺘﻀﺢ اﺜرﻫﺎ ﻓﻲ اﺨﺘﻔﺎء ﺘﻛوﻴن اﻟطﻴﺎ ارت ﻓﻲ ﺒﻌض اﺒﺎر
اﻟد ارﺴﺔ ﺨﺼوﺼﺎ ﻓﻲ اﺒﺎر ﺸرق ﻤﻴﺴﺎن .