青岛近海古河道断面特征与古地理变迁关系研究
|
摘要
通过对青岛近海1561km的高分辨率浅地层测量剖面解译,在多条剖面中发现研究区存在多期发育的古河道,虽然保存较完整的地层不多,但大部分河流亚相地层被保存。测年资料表明,这些河流多形成在37000～11000a之间,河流床底最大埋深(海底起算)约-32m,一般在-20～-28m,最大单个河面宽约1500m。根据现在所见河道的轮廓形态,可分为六种类型:即发育有滩心洲的河道、平底河道、不对称河道、连续多期发育的河道、窄陡型河道和对称型河道。并对河流的形成机理和古地理特征作了初步分析。
Based on high resolution seismic profiles surface of offshore 1 561 km nearby Qingdao, we discovered that there were multi-stage developed ancient river ways in this area and river sedimentary system was not well preserved in many stratums in the most of them only some of the river subfacies stratums are preserved. The character of river cross section to the east of 120°30′is relatively well preserved. The data of age measurement showed that these rivers were mostly formed 37 000～11 000 years ago, that the largest burial depth(from the bottom of modern sea to river bottom) of riverbed was about 32m and the usual burial depth was between 20～28 m and that the widest part of the river orientation was approximately 1 500 m. The river section can be divided into 6 types according to the present visible figures, which are watercourse developed with channel bar, flat base continuous multi-stage developed, steep narrow, asymmetric. This paper also includes the general analysis of formation mechanism of rivers and ancient geography environment.
Based on high resolution seismic profiles surface of offshore 1 561 km nearby Qingdao, we discovered that there were multi-stage developed ancient river ways in this area and river sedimentary system was not well preserved in many stratums in the most of them only some of the river subfacies stratums are preserved. The character of river cross section to the east of 120°30′is relatively well preserved. The data of age measurement showed that these rivers were mostly formed 37 000～11 000 years ago, that the largest burial depth(from the bottom of modern sea to river bottom) of riverbed was about 32m and the usual burial depth was between 20～28 m and that the widest part of the river orientation was approximately 1 500 m. The river section can be divided into 6 types according to the present visible figures, which are watercourse developed with channel bar, flat base continuous multi-stage developed, steep narrow, asymmetric. This paper also includes the general analysis of formation mechanism of rivers and ancient geography environment.
引文
1秦蕴珊.末次冰期以来陆架环境演化及沉积作用[J].大自然探索,1996,15(58)24-26[Qin Yunshan.Environmental evolution and sedi-mentation of continental shelf during the last glaciation[J].Exploration of Nature,1996,15(58):24-26]
2李凡,于建军,姜秀珩,等.南黄海埋藏古河系研究[J].海洋与湖沼,1991,22(6):501-508[Li Fan,Yu Jianjun,Jiang Xinheng,et al.Study on buried paleo-channel system in the south Yellow sea[J].Oceanologia et Limnologia Sinica,1991,22(6):501-508]
3刘洪宾.胶州湾成因的探讨[R].胶州湾开发与应用论文集,1985:129-132[Liu Hongbin.Discussion on the cause of formation of Jiaozhou Bay[R].The Proceeding of the Open and Application in Jiaozhou Bay,1985:129-132]
4栾光忠,刘红军,范德江.青岛胶州湾地质特征及其成因[J].海洋湖沼通报,1998,3:18-23[Luan Guangzhong,Liu Hongjun,Fan De-jiang.The geological feature and origin of the Jiaozhou Bay in Qingdao[J].Transactions of Oceanology and Limnology,1998,3:18-23]
5尹延鸿,薛春汀.山东崂山劈石口断裂的活动特征[J].海洋地质与第四纪地质,1987,7(1):123-127[Yin Yanhong,Xue Chunting,Character of Pishikou fracture activity in Shandong Laoshan[J].Ma-rine Geology and Quarternary Geology,1987,7(1):123-127]
6山东省第四地质矿产勘察院.山东省区域地质[M].北京:地质出版社,2003[Shandong Provincial No.4Institute of the Geological and Mineral Survey.Regional Geology in Shandong Province[M].Beijing:Geological Publishing House,2003]
7Reineck HE,Singh I B.陆源碎屑沉积环境[M].大庆油田科学研究设计院和江苏省地理研究所译.北京:石油工业出版社,1977:210-248[Depositional Environment of Fragmentary Matters of Terrige-nous[M].Translated by Daqing Institution of Petroleum Science&Jiangsu Institution of Geography.Beijing:Petroleum Industry Press,1977:210-248]
8Fahnestock R K.Morphology and hydrology of a glacial stream[J].U.S.Geology Survey Profess,1963:422-A,1-70
9Gould HR.密西西比河三角洲复合体[C]∥三角洲沉积译文集.地质矿产部海洋地质调查局译.上海:地质矿产部海洋地质调查局内部出版(总第32期),1985:1-13[Gould H R.Delta complexus in Mississippi river[C]∥The Proceedings of Delta Sediment.Translated by Marine Geological Survey Bureau.Ministry of Geology&Mineral Resources(Sum.No.32).,Shanghai,P.O.2d208,1985:1-13]
10William HK.得克萨斯州科罗拉多河三角洲岩相及发展史[C]∥三角洲沉积译文集.地质矿产部海洋地质调查局译,上海:地质矿产部海洋地质调查局内部出版(总第32期),1985:50-66[Wil-liam HK.Lithofacies and developed history of delta in Colorado river of Texas[C]∥The Proceedings of Delta Sediment.Translated by Ma-rine Geological Survey Bureau.Ministry of Geology&Mineral Re-sources(Sum.No.32).Shanghai,P.O.2d208,1985:50-66]
11刘宝-,等.沉积岩石学[M].北京:地质出版社,1980:357-377[Liu Baojun,et al.Lithology of Sedimentation[M].Beijing:Geolog-ical Publishing House,1980:357-377]
12Wright V P,Marriott S B.The sequence stratigraphy of fluvial deposi-tional systems:the role of floodplain sediment storage[J].Sedimentary Geology,1993,86:203-210
13Wright V P,Marriott S B.The sequence stratigraphy of fluvial deposi-tional systems:the role of floodplain sediment storage-reply[J].Sedi-mentary Geology,1994,92:289-290
14Meehan R L,Shlemon R J.The sequence stratigraphy of fluvial depo-sitional systems:the role of floodplain sediment storage:a comment[J].Sedimentary Geology,1994,92:287-288
15陈正新,姚长新,黄海燕,等.青岛近海浅层地震剖面解译中几种相位特征的地质意义探讨[J].海洋地质与第四纪地质,2007(增刊):119-124[Chen Zhengxin,Yao Changxin,Huang Haiyan,et al,Discussion on geological significance and judgment of several phase characteristics of offing shallow seismic section in Qingdao[J].Ma-rine Geology and Quaternary Geology,2007,27(Suppl.):119-124]
2李凡,于建军,姜秀珩,等.南黄海埋藏古河系研究[J].海洋与湖沼,1991,22(6):501-508[Li Fan,Yu Jianjun,Jiang Xinheng,et al.Study on buried paleo-channel system in the south Yellow sea[J].Oceanologia et Limnologia Sinica,1991,22(6):501-508]
3刘洪宾.胶州湾成因的探讨[R].胶州湾开发与应用论文集,1985:129-132[Liu Hongbin.Discussion on the cause of formation of Jiaozhou Bay[R].The Proceeding of the Open and Application in Jiaozhou Bay,1985:129-132]
4栾光忠,刘红军,范德江.青岛胶州湾地质特征及其成因[J].海洋湖沼通报,1998,3:18-23[Luan Guangzhong,Liu Hongjun,Fan De-jiang.The geological feature and origin of the Jiaozhou Bay in Qingdao[J].Transactions of Oceanology and Limnology,1998,3:18-23]
5尹延鸿,薛春汀.山东崂山劈石口断裂的活动特征[J].海洋地质与第四纪地质,1987,7(1):123-127[Yin Yanhong,Xue Chunting,Character of Pishikou fracture activity in Shandong Laoshan[J].Ma-rine Geology and Quarternary Geology,1987,7(1):123-127]
6山东省第四地质矿产勘察院.山东省区域地质[M].北京:地质出版社,2003[Shandong Provincial No.4Institute of the Geological and Mineral Survey.Regional Geology in Shandong Province[M].Beijing:Geological Publishing House,2003]
7Reineck HE,Singh I B.陆源碎屑沉积环境[M].大庆油田科学研究设计院和江苏省地理研究所译.北京:石油工业出版社,1977:210-248[Depositional Environment of Fragmentary Matters of Terrige-nous[M].Translated by Daqing Institution of Petroleum Science&Jiangsu Institution of Geography.Beijing:Petroleum Industry Press,1977:210-248]
8Fahnestock R K.Morphology and hydrology of a glacial stream[J].U.S.Geology Survey Profess,1963:422-A,1-70
9Gould HR.密西西比河三角洲复合体[C]∥三角洲沉积译文集.地质矿产部海洋地质调查局译.上海:地质矿产部海洋地质调查局内部出版(总第32期),1985:1-13[Gould H R.Delta complexus in Mississippi river[C]∥The Proceedings of Delta Sediment.Translated by Marine Geological Survey Bureau.Ministry of Geology&Mineral Resources(Sum.No.32).,Shanghai,P.O.2d208,1985:1-13]
10William HK.得克萨斯州科罗拉多河三角洲岩相及发展史[C]∥三角洲沉积译文集.地质矿产部海洋地质调查局译,上海:地质矿产部海洋地质调查局内部出版(总第32期),1985:50-66[Wil-liam HK.Lithofacies and developed history of delta in Colorado river of Texas[C]∥The Proceedings of Delta Sediment.Translated by Ma-rine Geological Survey Bureau.Ministry of Geology&Mineral Re-sources(Sum.No.32).Shanghai,P.O.2d208,1985:50-66]
11刘宝-,等.沉积岩石学[M].北京:地质出版社,1980:357-377[Liu Baojun,et al.Lithology of Sedimentation[M].Beijing:Geolog-ical Publishing House,1980:357-377]
12Wright V P,Marriott S B.The sequence stratigraphy of fluvial deposi-tional systems:the role of floodplain sediment storage[J].Sedimentary Geology,1993,86:203-210
13Wright V P,Marriott S B.The sequence stratigraphy of fluvial deposi-tional systems:the role of floodplain sediment storage-reply[J].Sedi-mentary Geology,1994,92:289-290
14Meehan R L,Shlemon R J.The sequence stratigraphy of fluvial depo-sitional systems:the role of floodplain sediment storage:a comment[J].Sedimentary Geology,1994,92:287-288
15陈正新,姚长新,黄海燕,等.青岛近海浅层地震剖面解译中几种相位特征的地质意义探讨[J].海洋地质与第四纪地质,2007(增刊):119-124[Chen Zhengxin,Yao Changxin,Huang Haiyan,et al,Discussion on geological significance and judgment of several phase characteristics of offing shallow seismic section in Qingdao[J].Ma-rine Geology and Quaternary Geology,2007,27(Suppl.):119-124]
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心