贺兰拗拉谷北段奥陶系等深流沉积
|
摘要
采用野外观察描述和室内分析相结合的方法,以桌子山剖面奥陶系沉积相研究为基础,识别出了典型的碳酸盐等深流沉积。首次采用Fischer图解法,求取了碳酸盐等深流沉积其可容空间变化曲线。参照野外的样品化学分析数据,得出深水等深岩的生烃能力较好,故对等深岩的研究具有潜在的矿产意义。在未来研究上,应运用地震波识别、遥感等现代科技调查手段,进行多学科综合研究,尽快建立一套完善的识别标志,以促使其逐渐成为沉积学中一个更为完善的研究领域。
Representative carbonate contourite is discovered based on field outcrop descriptions and laboratory analysis based on detailed study of Zhuozishan section.This paper gets the portion of the carbonate contourite with hypothetical Fischer diagram showing changes in accommodation space as a function of cycle number.Using the chemical data of field samples,it is found that the carbonate contourite in deep sea may yield hydrocarbon effectively.It is significant to find potential mineral from contourite study.In the future,we should synthesize multidisciplinary approaches such as identification of seismic wave and remote sensing etc.and establish some effective discriminating indicators so as to advance the research ulteriorly and make it a more perfect research field in the marine sedimentology.
Representative carbonate contourite is discovered based on field outcrop descriptions and laboratory analysis based on detailed study of Zhuozishan section.This paper gets the portion of the carbonate contourite with hypothetical Fischer diagram showing changes in accommodation space as a function of cycle number.Using the chemical data of field samples,it is found that the carbonate contourite in deep sea may yield hydrocarbon effectively.It is significant to find potential mineral from contourite study.In the future,we should synthesize multidisciplinary approaches such as identification of seismic wave and remote sensing etc.and establish some effective discriminating indicators so as to advance the research ulteriorly and make it a more perfect research field in the marine sedimentology.
引文
[1]Heezen B C,Hollister C D.The Face of the Deep[M].Ox-ford:Oxford University Press,1971.
[2]Faugeres J C,Stow D A V.Bottom-current-controlled Sedi-mentation:a Synthesis of the Contourite Problem[J].Sedi-mentary Geology,1993,82(1/4):287-290.
[3]Stow D A V.Distinguishing Between Fine-grained Turbiditesand Contourites on the Nova Scotian Deep Water Margin[J].Sedimentology,2006,26(3):371-387.
[4]Stow D A W,Piper D J W.Deep-water Fine-grained Sedi-ments:Facies Models[J].Geo Soc London Spec Pub,1984,15:611-645.
[5]Stow D A V.Deep Sea Processes of Sediment Transport andDeposition[C]∥Pye K.Sediment Transport and DepositionalProcesses.London:Blackwell Sci Pub,1994:257-291.
[6]Faugeres J C,Mezerais M L,Stow D A V.Contourite DriftTypes and Their Distribution in the North and South Atlan-tic Ocean Basins[J].Sedimentary Geology,1993,82(1/4):189-203.
[7]高振中,何幼斌,罗顺社,等.深水牵引流沉积—内潮汐、内波和等深流沉积研究[M].北京:科学出版社,1996.
[8]张兴阳,高振中,姚雪根.北大西洋洛克尔海槽东北部内波沉积——深水大型沉积物波成因的再解释[J].沉积学报,1999,17(3):464-472.
[9]高振中,何幼斌,李建明,等.我国发现内潮汐沉积[J].科学通报,1997,42(13):1418-1421.
[10]高振中,Eriksson K A.美国阿巴拉契亚山脉芬卡苏地区奥陶纪海底水道中的内潮汐沉积[J].沉积学报,1993,11(1):12-22.
[11]Gao Z Z,Eriksson K A.Internal-tide Deposits in an Ordovi-cian Submarine Channel:Previously Unrecognized Facies?[J].Geology,1991,19(7):734-737.
[12]段太忠,郭建华,高振中,等.华南古大陆边缘湘北九溪下奥陶统碳酸盐等深岩丘[J].地质学报,1990,64(2):131-143.
[13]许文彬,徐茂泉,孙美琴,等.深流沉积研究现状与展望[J].台湾海峡,2004,23(3):45-52.
[14]Nelson C H,Baraza J,Maldonado A.Mediterranean Under-current Sandy Contourites,Gulf of Cadiz,Spain[J].Sedimen-tary Geology,1993,82(1/4):103-131.
[15]Folk R,Moser G.Tricritical Dynamics at the Demixing--λTransition in3He-4He Mixtures[J].Journal of Low Tem-perature Physics,2008,150(5/6):689-709.
[16]Gonthier E G,Faugeres J C,Stow D A V.Contourite Faciesof the Faro Drift,Gulf of Cadiz[C]∥Stow D A V,Piper D JW.Fine-grained Sediments:Deep-Water Processes and Faci-es.London:Blackwell Scientific Publications,1984:275-292.
[17]Hotchkiss F S,Wunsch C.Internal Waves in Hudson Canyonwith Possible Geological Implications[J].Deep-seaResearch,1982,29(4):415-442.
[18]Hays J D,Imbrie J,Shackleton N J.Variation in the Earth sOrbit:Pacemaker of the Ice Ages[J].Science,1976,194:1121-1132.
[19]Dickson R,Kidd R B.Circulation in the Southern RockallTrough the Oceanographic Setting of Site[J].SedimentaryGeology,1982,71(7):126-132.
[20]Grotzinger J P.Cyclicity and Paleoenvironmental Dynamics,Rocknest Platform,Northwest Canada[J].Geological Society ofAmerica,1986,97(10):1208-1231.
[21]Hardie L A,Dunn P A,Goldhammer R K.Field and Model-ling Studies of Cambrian Carbonate Cycles,Virginia Appala-chians:Discussion[J].Journal of Sedimentary Research,1991,61(4):636-646.
[22]夏新宇,洪峰,赵林,等.烃源岩生烃潜力的恢复探讨——以鄂尔多斯盆地下奥陶统碳酸盐岩为例[J].石油与天然气地质,1998,19(4):307-312.
[23]Bein A,Weiler Y.The Cretaceous Talme Yafe Formation:aContour Current Shaped Sedimentary Prism of CalcareousDetritus at the Continental Margin of the Arabian Craton[J].Sedimentology,2006,23(4):511-532.
[2]Faugeres J C,Stow D A V.Bottom-current-controlled Sedi-mentation:a Synthesis of the Contourite Problem[J].Sedi-mentary Geology,1993,82(1/4):287-290.
[3]Stow D A V.Distinguishing Between Fine-grained Turbiditesand Contourites on the Nova Scotian Deep Water Margin[J].Sedimentology,2006,26(3):371-387.
[4]Stow D A W,Piper D J W.Deep-water Fine-grained Sedi-ments:Facies Models[J].Geo Soc London Spec Pub,1984,15:611-645.
[5]Stow D A V.Deep Sea Processes of Sediment Transport andDeposition[C]∥Pye K.Sediment Transport and DepositionalProcesses.London:Blackwell Sci Pub,1994:257-291.
[6]Faugeres J C,Mezerais M L,Stow D A V.Contourite DriftTypes and Their Distribution in the North and South Atlan-tic Ocean Basins[J].Sedimentary Geology,1993,82(1/4):189-203.
[7]高振中,何幼斌,罗顺社,等.深水牵引流沉积—内潮汐、内波和等深流沉积研究[M].北京:科学出版社,1996.
[8]张兴阳,高振中,姚雪根.北大西洋洛克尔海槽东北部内波沉积——深水大型沉积物波成因的再解释[J].沉积学报,1999,17(3):464-472.
[9]高振中,何幼斌,李建明,等.我国发现内潮汐沉积[J].科学通报,1997,42(13):1418-1421.
[10]高振中,Eriksson K A.美国阿巴拉契亚山脉芬卡苏地区奥陶纪海底水道中的内潮汐沉积[J].沉积学报,1993,11(1):12-22.
[11]Gao Z Z,Eriksson K A.Internal-tide Deposits in an Ordovi-cian Submarine Channel:Previously Unrecognized Facies?[J].Geology,1991,19(7):734-737.
[12]段太忠,郭建华,高振中,等.华南古大陆边缘湘北九溪下奥陶统碳酸盐等深岩丘[J].地质学报,1990,64(2):131-143.
[13]许文彬,徐茂泉,孙美琴,等.深流沉积研究现状与展望[J].台湾海峡,2004,23(3):45-52.
[14]Nelson C H,Baraza J,Maldonado A.Mediterranean Under-current Sandy Contourites,Gulf of Cadiz,Spain[J].Sedimen-tary Geology,1993,82(1/4):103-131.
[15]Folk R,Moser G.Tricritical Dynamics at the Demixing--λTransition in3He-4He Mixtures[J].Journal of Low Tem-perature Physics,2008,150(5/6):689-709.
[16]Gonthier E G,Faugeres J C,Stow D A V.Contourite Faciesof the Faro Drift,Gulf of Cadiz[C]∥Stow D A V,Piper D JW.Fine-grained Sediments:Deep-Water Processes and Faci-es.London:Blackwell Scientific Publications,1984:275-292.
[17]Hotchkiss F S,Wunsch C.Internal Waves in Hudson Canyonwith Possible Geological Implications[J].Deep-seaResearch,1982,29(4):415-442.
[18]Hays J D,Imbrie J,Shackleton N J.Variation in the Earth sOrbit:Pacemaker of the Ice Ages[J].Science,1976,194:1121-1132.
[19]Dickson R,Kidd R B.Circulation in the Southern RockallTrough the Oceanographic Setting of Site[J].SedimentaryGeology,1982,71(7):126-132.
[20]Grotzinger J P.Cyclicity and Paleoenvironmental Dynamics,Rocknest Platform,Northwest Canada[J].Geological Society ofAmerica,1986,97(10):1208-1231.
[21]Hardie L A,Dunn P A,Goldhammer R K.Field and Model-ling Studies of Cambrian Carbonate Cycles,Virginia Appala-chians:Discussion[J].Journal of Sedimentary Research,1991,61(4):636-646.
[22]夏新宇,洪峰,赵林,等.烃源岩生烃潜力的恢复探讨——以鄂尔多斯盆地下奥陶统碳酸盐岩为例[J].石油与天然气地质,1998,19(4):307-312.
[23]Bein A,Weiler Y.The Cretaceous Talme Yafe Formation:aContour Current Shaped Sedimentary Prism of CalcareousDetritus at the Continental Margin of the Arabian Craton[J].Sedimentology,2006,23(4):511-532.
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