Given sustaining exploration, the eastern zone of the Sulige gas field may soon become a key area of exploitation. In order to explore its genesis, types and distribution of the reservoir sandstones in the eastern zon...Given sustaining exploration, the eastern zone of the Sulige gas field may soon become a key area of exploitation. In order to explore its genesis, types and distribution of the reservoir sandstones in the eastern zone of this gas field, we focused in our study on the provenance and detailed sedimentary facies of sandstone of the He8 （the eighth part of the Shihezi formation, Permian system） and Shanxil （the first part of the Shanxi formation, Permian system） members, based on core observations, analyses in petrography, granularity and logging. The results show that： 1） the sandstone provenance of Shanxil and He8 in the eastern zone of the Sulige gas field is from the north of the Ordos Basin, characterized by dual directions from the north and northeast. 2） The He8 and Shanxil members were deposited in a fluvial-delta sedimentary system. The He8 was mainly deposited in braided rivers, in- cluding braided channels, channel bars, levee and floodplain sub-environments, whereas the Shanxil Member was deposited in braided rivers and deltas, including braided channels, channel bars, floodplains, tributaries and inter-tributary sub-environments. 3） Sedimentary facies bands migrated in drastic fashion towards the basin from the Shanxil to the He8 Member. Base levels of sedi- mentation generally present a trend of small increases in-amplitude, large decreasing amplitudes and slow and gradual Increases. 4） The continuity of the reservoir sandbodies along the source direction is better than that perpendicular to the direction. Compared with Shanxil, both dimensions and continuity of the sandbodies in He8 are better from which we conclude that it is the most fa- vorable part of the reservoir.展开更多
It is becoming an important controlling factor of gas exploration and exploitation in the east part of Sulige gas field in the Ordos Basin where the reservoir of main gas formations is tight sandstones. Employing expe...It is becoming an important controlling factor of gas exploration and exploitation in the east part of Sulige gas field in the Ordos Basin where the reservoir of main gas formations is tight sandstones. Employing experimental methods of slice identification, casting slice, scan electron microscope, and X-ray diffrac- tions, we studied the characteristics of petrology and diagenesis on reservoirs in Shanl section of Shanxi formation and He8 section of Shihezi formation of the Permian system in the East II part of Sulige gas field. The results include： （1） the main sandstones in these areas are dominated by lithic sandstone and litbic silicarenite with low grade of maturity; （2） the diagenesis of sandstone in these areas mainly include compaction, cementation, corrosion and alteration. Conclusions are as follows： （1） the diagenetic stage reached period B of the middle diagenetic stage; （2） the early diagenetic compaction is one of the main factors to decreasing porosity; （3） the secondary pores formed by corrosion in acidity medium con- ditions in period A of the middle diagenetic stage can distinctly ameliorate the poor reservoir capability of sandstone and, （4） cementation in period B of the middle diagenetic stage is the most important factor leading; to poor physical property of sandstone reservoirs.展开更多
Central Bilad al-Sudan refers to the areas of the ancient Hausa states, and the domains of the ancient Kanem Bornu. As a result of the aged long commercial, cultural, and religious linkages between North Africa and th...Central Bilad al-Sudan refers to the areas of the ancient Hausa states, and the domains of the ancient Kanem Bornu. As a result of the aged long commercial, cultural, and religious linkages between North Africa and the Central Sudan, one finds so many things in common among the two regions in dress, diets, cultural traits, as well as educational and religious practices. The extent of influence of the North African region on the individual and communal lives of the central Sudan has been extraordinarily great. The central Sudan is one of the most Islamized areas of West Africa, and Arabic language is second language to the Muslim communities in domestic and public spheres. And as a result of the entrenchment of Islam among the people due to the activities of North African scholars and traders the area became the hub of Islamic scholarship. The intellectual history of the Central Bilad al-Sudan cannot be complete without the mention of an Algerian scholar, Muhammad ibn Abd-A1-Kareem al-Maghili who in addition to his scholarly influence took appointment as Special Adviser in Kano in the 1460s. The same could be said of an Egyptian prolific writer, Jalal al-Deen al-Suyuti, who settled in Katsina and Gobir and also took the appointment of Grand Qadi in Katsina in the 15th century. Similarly, books of Sanhaja scholars, Shinqit Ulama＇a, as well as Spanish-Andalusian scholars via Morocco were made available and widely studied in this part of Muslim world. The combination of the activities of such scholars, literature, and learning tradition were responsible lbr the growth and development of Muslim intelligentsia in the central Bilad al-Sudan since the earliest time, and the influence continues to date. Thus this paper aims at examining the phenomenon, primarily by assessing the influence of scholars, literature, and educational institutions from the Maghreb on the intellectual development and the emergence of native scholars and intelligentsia and on the general scholarly trend in the central Bilad al-Sudan.展开更多
基金supported by the National Basic Re-search Program of China (No2003CB214603)
文摘Given sustaining exploration, the eastern zone of the Sulige gas field may soon become a key area of exploitation. In order to explore its genesis, types and distribution of the reservoir sandstones in the eastern zone of this gas field, we focused in our study on the provenance and detailed sedimentary facies of sandstone of the He8 （the eighth part of the Shihezi formation, Permian system） and Shanxil （the first part of the Shanxi formation, Permian system） members, based on core observations, analyses in petrography, granularity and logging. The results show that： 1） the sandstone provenance of Shanxil and He8 in the eastern zone of the Sulige gas field is from the north of the Ordos Basin, characterized by dual directions from the north and northeast. 2） The He8 and Shanxil members were deposited in a fluvial-delta sedimentary system. The He8 was mainly deposited in braided rivers, in- cluding braided channels, channel bars, levee and floodplain sub-environments, whereas the Shanxil Member was deposited in braided rivers and deltas, including braided channels, channel bars, floodplains, tributaries and inter-tributary sub-environments. 3） Sedimentary facies bands migrated in drastic fashion towards the basin from the Shanxil to the He8 Member. Base levels of sedi- mentation generally present a trend of small increases in-amplitude, large decreasing amplitudes and slow and gradual Increases. 4） The continuity of the reservoir sandbodies along the source direction is better than that perpendicular to the direction. Compared with Shanxil, both dimensions and continuity of the sandbodies in He8 are better from which we conclude that it is the most fa- vorable part of the reservoir.
基金supported by the Science Development Project of Shandong Province (No.2009GG20001021-07)the Open Fund of Shandong Provincial Key Laboratory of Depositional Mineralization & Sedimentary Minerals (No. DMSM200803)the SDUST Research Fund (No.2010KYTD103)
文摘It is becoming an important controlling factor of gas exploration and exploitation in the east part of Sulige gas field in the Ordos Basin where the reservoir of main gas formations is tight sandstones. Employing experimental methods of slice identification, casting slice, scan electron microscope, and X-ray diffrac- tions, we studied the characteristics of petrology and diagenesis on reservoirs in Shanl section of Shanxi formation and He8 section of Shihezi formation of the Permian system in the East II part of Sulige gas field. The results include： （1） the main sandstones in these areas are dominated by lithic sandstone and litbic silicarenite with low grade of maturity; （2） the diagenesis of sandstone in these areas mainly include compaction, cementation, corrosion and alteration. Conclusions are as follows： （1） the diagenetic stage reached period B of the middle diagenetic stage; （2） the early diagenetic compaction is one of the main factors to decreasing porosity; （3） the secondary pores formed by corrosion in acidity medium con- ditions in period A of the middle diagenetic stage can distinctly ameliorate the poor reservoir capability of sandstone and, （4） cementation in period B of the middle diagenetic stage is the most important factor leading; to poor physical property of sandstone reservoirs.
文摘Central Bilad al-Sudan refers to the areas of the ancient Hausa states, and the domains of the ancient Kanem Bornu. As a result of the aged long commercial, cultural, and religious linkages between North Africa and the Central Sudan, one finds so many things in common among the two regions in dress, diets, cultural traits, as well as educational and religious practices. The extent of influence of the North African region on the individual and communal lives of the central Sudan has been extraordinarily great. The central Sudan is one of the most Islamized areas of West Africa, and Arabic language is second language to the Muslim communities in domestic and public spheres. And as a result of the entrenchment of Islam among the people due to the activities of North African scholars and traders the area became the hub of Islamic scholarship. The intellectual history of the Central Bilad al-Sudan cannot be complete without the mention of an Algerian scholar, Muhammad ibn Abd-A1-Kareem al-Maghili who in addition to his scholarly influence took appointment as Special Adviser in Kano in the 1460s. The same could be said of an Egyptian prolific writer, Jalal al-Deen al-Suyuti, who settled in Katsina and Gobir and also took the appointment of Grand Qadi in Katsina in the 15th century. Similarly, books of Sanhaja scholars, Shinqit Ulama＇a, as well as Spanish-Andalusian scholars via Morocco were made available and widely studied in this part of Muslim world. The combination of the activities of such scholars, literature, and learning tradition were responsible lbr the growth and development of Muslim intelligentsia in the central Bilad al-Sudan since the earliest time, and the influence continues to date. Thus this paper aims at examining the phenomenon, primarily by assessing the influence of scholars, literature, and educational institutions from the Maghreb on the intellectual development and the emergence of native scholars and intelligentsia and on the general scholarly trend in the central Bilad al-Sudan.
