Application of natural gamma energy spectrum method for paleobathymetric recovery during carbonate deposition: A case study of M55 sub-member of Guanjiaya section in Xing County of Shanxi Province
-
摘要: 古水深分析对还原古环境与盆地构造演化历史具有重要的意义。目前古水深恢复多以定性为主,对样品可靠性的要求较高,且易受资料条件限制,而自然伽马能谱法具有易获取、成本低、受控因素少等优点,可结合水深函数半定量恢复水深,但该方法多被用于陆相碎屑岩的研究中,是否适用于海相碳酸盐岩尚需验证。以鄂尔多斯盆地关家崖剖面奥陶系马家沟组五5亚段为例,利用自然伽玛能谱法恢复了碳酸盐岩沉积时的古水深,恢复结果与碳同位素法、生物遗迹法、岩石组构法显示的结果一致。研究验证了自然伽马能谱法在恢复碳酸盐岩沉积时的古水深方面具有较高的可信度与实用性。Abstract: The paleobathymetric analysis is of great significance to the paleoenvironment reconstruction and tectonic evolution of the basin. At present, paleobathymetric recovery is mainly qualitative, with high requires of sample reliability and is easy to be limited by the data condition. The natural gamma energy spectrum method has the advantages of accessiblity, low cost and few controlled factors, and can be used to semi-quantitative paleobathymetric recovery based on bathymetric function. However, this method is mostly used in terrestrial clastic rock deposition and its suitability for marine carbonate rock deposition is not clear. Taking the M55 sub-member of Ordovician Majiagou Formation in Guanjiaya section of Ordos Basin as an example, the authors in this paper used the natural gamma energy spectrum method to reconstruct the paleobathymetry of carbonate sediments. This method has good consistency and same results obtained by carbon isotopic method, biological heritage method and rock fabric method. The credibility and practicability of natural gamma energy spectrum method in recovering paleobathymetric recovery was also proven.
-
-
[1] 张才利,高阿龙,刘哲,等.鄂尔多斯盆地长7油层组沉积水体及古气候特征研究[J].天然气地球科学,2011,22(4):582-587.
[2] Zhang C L,Gao A L,Liu Z,et al.Study of character on sedimentary water and palaeoclimate for Chang7 oil layer in Ordos Basin[J].Natural Gas Geoscience,2011,22(4):582-587.
[2] 郭秋麟,倪丙荣.利用化石群分异度探讨古水深[J].石油大学学报:自然科学版,1990,14(2):1-7.
[4] Guo Q L,Ni B R.Determination of palaeodepth with diversity of fossil community[J].Journal of the University of Petroleum,China,1990,14(2):1-7.
[3] 赵澂林,姜在兴,刘孟慧.东濮凹陷西部下第三系的遗迹相[J].石油大学学报:自然科学版,1989,13(1):1-8.
[6] Zhao C L,Jiang Z X,Liu M H.Ichnofacies of the Eocene in western Dongpu depression[J].Journal of the University of Petro-leum,China,1989,13(1):1-8.
[4] van der Zwaan G J,Jorissen F J,De Stigter H C.The depth dependency of planktonic/benthic foraminiferal ratios:Constraints and applications[J].Marine Geology,1990,95(1):1-16.
[5] Ginsburg R N,Rezak R,Wray J L.Geology of Calcareous Algae:Notes for A Short Course[R].Miami:University of Miami,1971.
[6] 王成善,李祥辉.沉积盆地分析原理与方法[M].北京:高等教育出版社,2003.
[10] Wang C S,Li X H.Sedimentary Basin:From Principles to Analyses[M].Beijing:Higher Education Press,2003.
[7] 康波,解习农,杜学斌,等.基于滨线轨迹的古水深定量计算新方法——以古近系沙三中段东营三角洲为例[J].沉积学报,2012,30(3):443-450.
[12] Kang B,Xie X N,Du X B,et al.A new paleobathymetric approach based on shoreline trajectory:An example from Dongying delta in the third member of Paleogene Shahejie Formation[J].Acta Sedimentologica Sinica,2012,30(3):443-450.
[8] 董刚,何幼斌.根据地层厚度恢复古水深的研究[J].长江大学学报:自然科学版,2010,7(3):484-486.
[14] Dong G,He Y B.Study on paleo-water-depth restoration according based on stratum thickness[J].Journal of Yangtze University:Natural Science Edition,2010,7(3):484-486.
[9] 庞军刚,李文厚,肖丽.陕北地区延长组坳陷湖盆浅湖与深湖亚相的识别特征[J].兰州大学学报:自然科学版,2009,45(6):36-40.
[16] Pang J G,Li W H,Xiao L.Identifying characteristics of shallow lake and deep lake of Yanchang Formation depressed type lacustrine basin in Shanbei area[J].Journal of Lanzhou University:Natural Sciences,2009,45(6):36-40.
[10] 钟建华,倪良田,邵珠福,等.渤海湾盆地古近纪超深水与极超深水沉积及油气地质意义[J].高校地质学报,2017,23(3):521-532.
[18] Zhong J H,Ni L T,Shao Z F,et al.Identification of the ultra deep water deposition of the Bohai Bay Basin during the Paleogene and its significance for oil and gas geology[J].Geological Journal of China Universities,2017,23(3):521-532.
[11] 田景春,曾允孚.贵州二叠纪海相碳酸盐岩碳、氧同位素地球化学演化规律[J].成都理工学院学报,1995,22(1):78-82.
[20] Tian J C,Zeng Y F.The evolution pattern of the carbon and oxygen isotopes in the Permian marine carbonate rocks from Guizhou[J].Journal of Chengdu University of Technology,1995,22(1):78-82.
[12] 许中杰,蓝艺植,程日辉,等.句容地区下奥陶统仑山组海平面变化的碳酸盐岩地球化学记录[J].吉林大学学报:地球科学版,2017,47(5):1458-1470.
[22] Xu Z J,Lan Y Z,Cheng R H,et al.Carbonate geochemical record of sea-level change of Lunshan Formation in Lower Ordovician in Jurong area[J].Journal of Jilin University:Earth Science Edition,2017,47(5):1458-1470.
[13] 邵龙义,Jones T P.桂中晚二叠世碳酸盐岩碳同位素的地层学意义[J].沉积学报,1999,17(1):84-88.
[24] Shao L Y,Jones T P.Carbon isotopes and the stratigraphical implication of the Late Permian carbonates in central Guangxi[J].Acta Sedimentologica Sinica,1999,17(1):84-88.
[14] 汪凯明,罗顺社.碳酸盐岩地球化学特征与沉积环境判别意义——以冀北坳陷长城系高于庄组为例[J].石油与天然气地质,2009,30(3):343-349.
[26] Wang K N,Luo S S.Geochemical characters of carbonates and indicative significance of sedimentary environment:An example from the Gaoyuzhuang Formation of the Changcheng System in the northern Hebei depression[J].Oil & Gas Geology,2009,30(3):343-349.
[15] 李任伟,陈锦石,张淑坤.中元古代雾迷山组碳酸盐岩碳和氧同位素组成及海平面变化[J].科学通报,1999,44(16):1697-1702.
[28] Li R W,Chen J S,Zhang S K.Carbon and oxygen isotope composition of the carbonale rocks and its implication for sea-level change of Middle Proterozoic Wumishang Formation[J].Chinese Science Bulletin,1999,44(16):1697-1702.
[16] 许中杰,孔锦涛,程日辉,等.下扬子南京地区早寒武世幕府山组海平面相对升降的地球化学和碳、氧同位素记录[J].吉林大学学报:地球科学版,2020,50(1):158-169.
[30] Xu Z J,Kong J T,Cheng R H,et al.Geochemical and carbon and oxygen isotope records of relative sea-level change of Mufushan Formation in Early Cambrian in Nanjing,Lower Yangtze Region[J].Journal of Jilin University:Earth Science Edition,2020,50(1):158-169.
[17] 刘鑫,尚婷,田景春,等.鄂尔多斯盆地镇北地区延长组长4+5段沉积期古环境条件及意义[J].地质学报,2021,95(11):3501-3518.
[32] Liu X,Shang T,Tian J C,et al.Paleo-sedimentary environmental conditions and its significance of Chang 4+5 member of Triassic Yanchang Formation in the Zhenbei area,Ordos Basin,NW China[J].Acta Geologica Sinica,2021,95(11):3501-3518.
[18] Emmel B,De Jager G,Zieba K,et al.A 3D,map based approach to reconstruct and calibrate Palaeo-bathymetries - testing the cretaceous water depth of the Hammerfest Basin,southwestern Barents Sea[J].Continental Shelf Research,2015,97:21-31.
[19] 李佳穆. 地球化学测井在松科二井古环境分析中的应用[D].北京:中国地质大学(北京),2021.
[35] Li J M.Application of Geochemical Logging in Paleoenvironment Analysis of Well SK-2[D].Beijing:China University of Geosciences (Beijing),2021.
[20] 彭诚. 松辽盆地科探井古环境古气候测井分析方法及其关键问题研究[D].北京:中国地质大学(北京),2019.
[37] Peng C.Research on Log Analysis Method of Paleoenvironmentand Paleoclimate from Scientific Drilling Boreholes in Songliao Basin and Its Key Issues[D].Beijing:China University of Geosciences (Beijing),2019.
[21] 徐论勋. 晋西兴县奥陶系石油地质综合研究[M].北京:石油工业出版社,2004.
[39] Xu L X.Comprehensive Study of Ordovician Petroleum Geology in Xingxian County,Jinxi[M].Beijing:Petroleum Industry Press,2004.
[22] 杜江民,张小莉,聂万才,等.苏里格地区马五5亚段储集层特征及其主控因素[J].新疆石油地质,2017,38(1):34-40.
[41] Du J M,Zhang X L,Nie W C,et al.Study on reservoir characteristics and main controlling factors of Ma-55 submember in Sulige area[J].Xinjiang Petroleum Geology,2017,38(1):34-40.
[23] 宁博,王起琮,李百强,等.鄂尔多斯盆地马五-5亚段白云岩化成因模式[J].新疆石油地质,2015,36(5):531-538.
[43] Ning B,Wang Q C,Li B Q,et al.Genetic model for M5-5 submember dolomitization of Majiegou Formation in Ordos Basin[J].Xinjiang Petroleum Geology,2015,36(5):531-538.
[24] 史基安,邵毅,张顺存,等.鄂尔多斯盆地东部地区奥陶系马家沟组沉积环境与岩相古地理研究[J].天然气地球科学,2009,20(3):316-324.
[45] Shi J A,Shao Y,Zhang S C,et al.Lithofacies paleogeography and sedimentary environment in Ordovician Majiagou Formation,eastern Ordos Basin[J].Natural Gas Geoscience,2009,20(3):316-324.
[25] 包洪平,杨承运.鄂尔多斯东部奥陶系马家沟组微相分析[J].古地理学报,2000,2(1):31-42.
[47] Bao H P,Yang C Y.Study on microfacies of Majiagou Formation,Lower Ordovician,eastern Ordos,North China[J].Journal of Palaeogeography,2000,2(1):31-42.
[26] 黄道军,佘伟,魏柳斌,等.运用岩石组构、生物遗迹及地球化学重建碳酸盐岩沉积古环境——以山西兴县关家崖马五-5亚段为例[J].成都理工大学学报:自然科学版,2021,48(5):539-548.
[49] Huang D J,She W,Wei L B,et al.Reconstruction of carbonate sedimentary palaeo-environment by using rock fabric,biological remains and geochemistry:A case study of the Ma 5-5 submember at Guanjiaya,Xingxian,Shanxi,China[J].Journal of Chengdu University of Technology:Science & Technology Edition,2021,48(5):539-548.
[27] 陈中红,查明,金强.自然伽玛及自然伽玛能谱测井在沉积盆地古环境反演中的应用[J].地球物理学报,2004,47(6):1145-1150.
[51] Chen Z H,Zha M,Jin Q.Application of natural gamma ray logging and natural gamma spectrometry logging to recovering paleoenvironment of sedimentary basin[J].Chinese Journal of Geophysics,2004,47(6):1145-1150.
[28] 冯伟明,谢渊,刘建清,等.海相碳酸盐岩自然伽马能谱测井资料的沉积学意义——以川东南L1井下寒武统清虚洞组为例[J].海洋地质与第四纪地质,2016,36(5):165-172.
[53] Feng W M,Xie Y,Liu J Q,et al.Sedimentological significance of natural gamma ray logging data of marine carbonate:A case of the well L1 of Qingxudong Formation,Lower Cambrian in southeast Sichuan Basin[J].Marine Geology & Quaternary Geology,2016,36(5):165-172.
[29] 高达,林畅松,胡明毅,等.利用自然伽马能谱测井识别碳酸盐岩高频层序——以塔里木盆地塔中地区T1井良里塔格组为例[J].沉积学报,2016,34(4):707-715.
[55] Gao D,Lin C S,Hu M Y,et al.Using spectral gamma ray log to recognize high-frequency sequences in carbonate strata:A case study from the Lianglitage Formation from Well T1 in Tazhong area,Tarim Basin[J].Acta Sedimentologica Sinica,2016,34(4):707-715.
[30] 阳孝法,林畅松,杨海军,等.自然伽马能谱在塔中地区晚奥陶世碳酸盐岩层序地层分析中的应用[J].石油地球物理勘探,2010,45(3):384-391.
[57] Yang X F,Lin C S,Yang H J,et al.Application of natural gamma ray spectrometry in analysis of Late Ordovician carbonate sequence stratigraphic analysis in middle Tarim Basin[J].Oil Geophysical Prospecting,2010,45(3):384-391.
[31] Udchachon M,Thassanapak H,Feng Q L,et al.Palaeoenvironmental implications of geochemistry and radiolarians from Upper Devonian chert/shale sequences of the Truong Son fold belt,Laos[J].Geological Journal,2017,52(1):154-173.
[32] Wignall P B,Twitchett R J.Oceanic anoxia and the end Permian mass extinction[J].Science,1996,272(5265):1155-1158.
[33] 陈中红,查明.铀曲线在沉积盆地古环境反演中的应用[J].石油大学学报:自然科学版,2004,28(6):11-15.
[61] Chen Z H,Zha M.Application of uranium curve to paleoenvironment inversion in sedimentary basin[J].Journal of the University of Petroleum,China,2004,28(6):11-15.
[34] Derry L A,Brasier M D,Corfield R M,et al.Sr and C isotopes in Lower Cambrian carbonates from the Siberian Craton:A paleoenvironmental record during the “Cambrian explosion”[J].Earth and Planetary Science Letters,1994,128(3/4):671-681.
[35] Kaufman A J,Knoll A H.Neoproterozoic variations in the C-isotopic composition of seawater:stratigraphic and biogeochemical implications[J].Precambrian Research,1995,73(1/2/3/4):27-49.
[36] 黄思静. 碳酸盐岩的成岩作用[M].北京:地质出版社,2010:288.
[65] Huang S J.Carbonate Diagenesis[M].Beijing:Geology Press,2010:288.
[37] 刘梦瑶,史云鹤,董国栋,等.山西兴县中奥陶统马家沟组五5亚段遗迹化石组合及其古环境意义[J].古生物学报,2019,58(4):487-501.
[67] Liu M Y,Shi Y H,Dong G D,et al.Characteristics of paleoenvironmental evolution and ichnocoenosis in the 55 submember of the Middle Ordovician Majiagou Formation,Xingxian,Shanxi[J].Acta Palaeontologica Sinica,2019,58(4):487-501.
[38] 杨式溥. 遗迹化石的古环境和古地理意义[J].古地理学报,1999,1(1):7-19.
[69] Yang S P.Palaeoenvironmental and palaeogeographic significance of trace fossils[J].Journal of Palaeogeography,1999,1(1):7-19.
[39] Ekdale A A,Mason T R.Characteristic trace-fossil associations in oxygen-poor sedimentary environments[J].Geology,1988,16(8):720-723.
-
计量
- 文章访问数: 475
- PDF下载数: 87
- 施引文献: 0
下载: