«上一篇/Previous Article|本期目录/Table of Contents|下一篇/Next Article»

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:

第45卷

期数:

2023年第03期

页码:

653-662

栏目:

沉积地质与油气勘探

出版日期:

2023-05-15

文章信息/Info

Title:

Modern Sedimentary Characteristics and Sedimentary Evolution of Barrier-type Coast in Yudai Beach of Hainan, China

文章编号:

1672-6561(2023)03-0653-10

作者:

唐明远¹; 雷 涛¹; 高青松¹; 陈 奎¹; 任广磊¹; 刘林松¹; 赵永刚^2*

(1. 中国石化华北油气分公司勘探开发研究院,河南 郑州 450006; 2. 西安石油大学 地球科学与工程学院,陕西 西安 710065)

Author(s):

TANG Ming-yuan¹;  LEI Tao¹;  GAO Qing-song¹;  CHEN Kui¹;  REN Guang-lei¹;  LIU Lin-song¹;  ZHAO Yong-gang^2*

(1. Exploration & Development Research Institute, North China Oil and Gas Company, SINOPEC, Zhengzhou 450006, Henan, China; 2. School of Earth Sciences and Engineering, Xi'an Shiyou University, Xi'an 710065, Shaanxi, China)

关键词:

沉积学;  障壁岛;  潟湖;  河口沙坝;  冲积岛;  潮汐通道;  演化;  海南

Keywords:

sedimentology;  barrier island;  lagoon;  estuary sandbar;  alluvial island;  tidal channel;  evolution;  Hainan

分类号:

P931; P531

DOI:

10.19814/j.jese.2022.11019

文献标志码:

A

摘要:

海南玉带滩是我国南海沿岸典型的障壁型海岸现代沉积场所之一。根据野外考察和室内分析,从沉积物的成分、结构、沉积构造等方面揭示了玉带滩障壁型海岸现代沉积特征。结果表明:玉带滩东侧为障壁岛海滩,沉积层序总体上表现为粒度向上变粗; 中部为障壁岛沙丘,以中、粗粒石英砂为主,具平行层理、斜层理; 西侧为障壁坪,以中、细砂沉积为主,夹杂一些贝壳碎片,层理构造比较明显。玉带滩西侧水体为河流作用明显强于潮汐作用的潟湖; 河口沙坝发育或河流岩岛阻挡产生河汊是形成潟湖中冲积岛分布的主要原因; 仅在潮汐通道外侧出现拦口沙坝堆积。现代沉积特征结合Google Earth卫星图像分析认为,该障壁型海岸沉积演化大致包括3个阶段:第一阶段,河流携带泥沙入海,在河口湾地区形成多级近新月型河口沙坝。第二阶段,由于后期水道延伸方向、水动力的不断变化,西侧河口沙坝出现合并并向冲积岛转化; 在海岸拐弯处,以原有河口沙坝为主体,形成初期障壁沙坝,障壁沙坝西侧水体演变成潟湖。第三阶段,障壁岛西侧受河流冲刷作用影响,河口沙坝坝头几乎完全消失; 障壁沙坝形成后,潟湖水面加宽,流速减小,河口沙坝增生合并,最终形成了三大冲积岛(沙坡岛、东屿岛、鸳鸯岛)。该障壁型海岸现代沉积发育冲积岛的障壁岛-潟湖沉积体系,而不同于传统的碎屑海岸障壁岛-潟湖沉积体系,研究其沉积特征和沉积演化为进一步认识和预测特殊类型的古代碎屑海岸障壁岛-潟湖沉积体系油气储层提供了具有参考价值的沉积演化模式。

Abstract:

Yudai beach in Hainan is one of the typical modern barrier-type coast sedimentary sites along the South China Sea coast. According to the field investigation and laboratory research, the modern sedimentary characteristics of barrier-type coast of Yudai beach were revealed from the the composition, structure and sedimentary structure of the sediments. The results show that the east side of Yudai beach is the barrier island beach, and on the whole, the grain size of sedimentary sequence becomes coarser from bottom to top; the middle part is the barrier island sand dunes, mainly with medium and coarse grained quartz sand, parallel bedding and oblique bedding; the west side is the barrier flat, the sediment is mainly medium and fine sand with some shell fragments, and the bedding structure is obvious. The waters on the west side of Yudai beach are lagoons with stronger river action than tidal action. The main reason for the distribution of alluvial islands in lagoons is the development of estuary sandbar or river branch generated by the obstruction of river rock islands. Only the estuary sandbar accumulation occurs outside the tidal channel. According to modern sedimentary characteristics and the satellite remote sensing images of Google Earth, the barrier-type coastal sedimentary evolution includes three stages: ① The river carries sediment into the sea, forming a multi-stage approximate crescent estuary sandbar in the estuary region. ② Due to the continuous changes in the extension direction of the waterway and hydrodynamic force in the later period, the sandbars in the western estuary are merged and transformed into alluvial islands; at the turning area of the coast, the original estuary sandbars are taken as the main body to form the initial barrier sandbars, and the water on the west side of the barrier sandbars evolve into lagoons. ③ The west side of barrier island is affected by river scouring, and the head of estuary sandbar almost completely disappears; after the barrier island sandbar formed, the lagoon water surface widens, the flow velocity decreases, and the estuary sandbar proliferates and merges, and finally three major alluvial islands(Shapo island, Dongyu island and Yuanyang island)are formed. The barrier-type coast modern sedimentation is a barrier island-lagoon sedimentary system with alluvial island, which is different from the traditional clastic coastal barrier island-lagoon sedimentary system. Study on the sedimentary characteristics and evolution has provided a valuable sedimentary evolution model for further understanding and predicting the oil and gas reservoirs of the ancient clastic coastal barrier island-lagoon sedimentary system.

参考文献/References:

[1] 郭英海,李壮福,张德高,等.海南岛万宁小海的障壁海岸沉积[J].中国矿业大学学报,1999,28(5):461-464.
GUO Ying-hai,LI Zhuang-fu,ZHANG De-gao,et al.Barrier Coast Deposition in Wanning Xiaohai of Hai-nan Island[J].Journal of China University of Mining & Technology,1999,28(5):461-464.
[2] 庄振业,李从先.山东半岛滨外坝沙体沉积特征[J].海洋学报,1989,11(4):470-480.
ZHUANG Zhen-ye,LI Cong-xian.Sedimentary Cha-racteristics of Offshore Bar Sand Bodies in Shandong Peninsula[J].Acta Oceanologica Sinica,1989,11(4):470-480.
[3] 魏合龙,庄振业.山东荣成湾月湖地区的潟湖-潮汐汊道体系[J].湖泊科学,1997,9(2):135-140.
WEI He-long,ZHUANG Zhen-ye.Study on the Evolution of Yuehu Lake-tidal Inlet System,Rongcheng Bay,Shandong Province[J].Journal of Lake Sciences,1997,9(2):135-140.
[4] 李晓路,于兴河,谭程鹏,等.潮汕地区全新世障壁海岸三角洲沉积演化与砂体展布[J].沉积学报,2015,33(4):706-712.
LI Xiao-lu,YU Xing-he,TAN Cheng-peng,et al.Se-dimentary Evolution and Sand-body Distribution of Holocene Period,Barrier Coast Delta,Chaoshan Region[J].Acta Sedimentologica Sinica,2015,33(4):706-712.
[5] 季汉成,赵澄林,谢庆宾.现代沉积[M].2版.北京:石油工业出版社,2004.
JI Han-cheng,ZHAO Cheng-lin,XIE Qing-bin.Mo-dern Sedimentation[M].2nd ed.Beijing:Petroleum Industry Press,2004.
[6] 庞军刚,李文厚,杨友运,等.鄂尔多斯盆地子洲地区上古生界沉积体系特征[J].天然气工业,2007,27(12):58-61,164.
PANG Jun-gang,LI Wen-hou,YANG You-yun,et al.Features of Upper Paleozoic Depositional System in Zizhou Region,Ordos Basin[J].Natural Gas Industry,2007,27(12):58-61,164.
[7] 马 瑶,李文厚,王若谷,等.鄂尔多斯盆地子洲地区上古生界沉积相及演化特征[J].地质科学,2015,50(1):286-302.
MA Yao,LI Wen-hou,WANG Ruo-gu,et al.Sedimentary Facies and Its Evolution of the Upper Palaeo-zoic in Zizhou Area of Ordos Basin[J].Chinese Journal of Geology,2015,50(1):286-302.
[8] 于兴河,王香增,王念喜,等.鄂尔多斯盆地东南部上古生界层序地层格架及含气砂体沉积演化特征[J].古地理学报,2017,19(6):935-954.
YU Xing-he,WANG Xiang-zeng,WANG Nian-xi,et al.Sequence Stratigraphic Framework and Sedimentary Evolution Characteristics of Gas-bearing Sandbody in the Upper Paleozoic in Southeastern Ordos Basin[J].Journal of Palaeogeography(Chinese Edition),2017,19(6):935-954.
[9] 侯中帅,陈世悦,王 越,等.鄂尔多斯盆地东缘保德地区上古生界层序地层与沉积相特征[J].古地理学报,2018,20(2):231-243.
HOU Zhong-shuai,CHEN Shi-yue,WANG Yue,et al.Characteristics of Sequence Stratigraphy and Sedimentary Facies of the Upper Paleozoic in Baode Area,Eastern Margin of Ordos Basin[J].Journal of Palaeogeography(Chinese Edition),2018,20(2):231-243.
[10] 刘 畅.鄂尔多斯盆地临兴地区上古生界层序地层格架及沉积模式[J].非常规油气,2019,6(1):23-33.
LIU Chang.Sequence Stratigraphy Framework and Sedimentary Model of Upper Paleozoic in Linxing Area,Ordos Basin[J].Unconventional Oil & Gas,2019,6(1):23-33.
[11] LI Y,GAO X D,MENG S Z,et al.Diagenetic Sequences of Continuously Deposited Tight Sandstones in Various Environments:A Case Study from Upper Paleozoic Sandstones in the Linxing Area,Eastern Ordos Basin,China[J].AAPG Bulletin,2019,103(11):2757-2783.
[12] LI Y,WANG Z S,WU P,et al.Paleoenvironment Reconstruction of the Upper Paleozoic in the Linxing Area,Northeastern Ordos Basin,China[J].AAPG Bulletin,2021,105(12):2545-2574.
[13] 郝蜀民,李 良,尤欢增.大牛地气田石炭—二叠系海陆过渡沉积体系与近源成藏模式[J].中国地质,2007,34(4):606-611.
HAO Shu-min,LI Liang,YOU Huan-zeng.Permo-Carboniferous Paralic Depositional Systems in the Daniudi Gas Field and Its Near-source Box-type Gas Accumulation-forming Model[J].Geology in China,2007,34(4):606-611.
[14] 郑文波,胡向阳,陈舒薇,等.鄂尔多斯盆地大牛地气田上古生界沉积演化特征[J].沉积学报,2015,33(2):306-313.
ZHENG Wen-bo,HU Xiang-yang,CHEN Shu-wei,et al.Characteristics of Sedimentary Evolution in the Upper Paleozoic,Daniudi Gasfield,Ordos Basin[J].Acta Sedimentologica Sinica,2015,33(2):306-313.
[15] 杨辰雨,田景春,张 翔,等.基于砂体构型精细刻画潮坪砂坝优质砂体:以大牛地气田D17井区太原组2段为例[J].石油与天然气地质,2015,36(2):248-254.
YANG Chen-yu,TIAN Jing-chun,ZHANG Xiang,et al.Configuration-based Fine Description of High-quality Sand Bodies in Tidal-flat Bar:Taking the Tight Sandstone Reservoir in the 2nd Member of the Taiyuan Formation in D17 Wellblock,Daniudi Gasfield as an Example[J].Oil & Gas Geology,2015,36(2):248-254.
[16] 刘林松,何发岐,雷 涛,等.DND气田D17区太2段障壁砂坝砂体精细刻画[J].西安石油大学学报(自然科学版),2022,37(增2):45-50.
LIU Lin-song,HE Fa-qi,LEI Tao,et al.Fine Characterization for Barrier Bar Sandbodies of T2 Group in D17 Block,DND Gas Field[J].Journal of Xi'an Shi-you University(Natural Science Edition),2022,37(S2):45-50.
[17] 郭艳琴,王美霞,郭彬程,等.鄂尔多斯盆地西缘北部上古生界沉积体系特征及古地理演化[J].西北大学学报(自然科学版),2020,50(1):93-104.
GUO Yan-qin,WANG Mei-xia,GUO Bin-cheng,et al.Sedimentary System Characteristics and Paleographic Evolution of Upper Paleozoic of Northern West Margin,Ordos Basin[J].Journal of Northwest University(Natural Science Edition),2020,50(1):93-104.
[18] 郭艳琴,赵灵生,郭彬程,等.鄂尔多斯盆地及周缘地区下二叠统沉积特征[J].古地理学报,2021,23(1):65-80.
GUO Yan-qin,ZHAO Ling-sheng,GUO Bin-cheng,et al.Sedimentary Characteristics of the Lower Permian in Ordos Basin and Its Adjacent Areas[J].Journal of Palaeogeography(Chinese Edition),2021,23(1):65-80.
[19] 殷 勇,朱大奎,唐文武,等.博鳌地区沙坝-潟湖沉积及探地雷达的应用[J].地理学报,2002,57(3):301-309.
YIN Yong,ZHU Da-kui,TANG Wen-wu,et al.On Barrier-lagoon Development and GPR Application in Bo'ao Area[J].Acta Geographica Sinica,2002,57(3):301-309.
[20] 王 洁,吴创收,杨世伦,等.海南博鳌玉带沙海滩冲淤演变及脆弱性分析[J].上海国土资源,2011,32(3):41-45.
WANG Jie,WU Chuang-shou,YANG Shi-lun,et al.Vulnerability Analysis and Scouring & Silting Evol-vement of Yudaisha Beach in Bo'ao,Hainan Island[J].Shanghai Land & Resources,2011,32(3):41-45.
[21] 程 林,田海兰,刘西汉,等.近44年来滦河口障壁岛演变过程及其影响因素研究:以唐山市龙岛为例[J].海洋科学,2020,44(6):22-30.
CHENG Lin,TIAN Hai-lan,LIU Xi-han,et al.Variations and Influencing Factors of the Barrier Islands near the Luan River Estuary in the Past 44 Years:A Case Study of the Loong Island in Tangshan[J].Marine Sciences,2020,44(6):22-30.
[22] 殷 勇,朱大奎,关洪军,等.应用探地雷达方法对海南岛博鳌海岸沙坝的研究[J].海洋地质与第四纪地质,2002,22(3):119-127.
YIN Yong,ZHU Da-kui,GUAN Hong-jun,et al.Application of Ground-penetrating-radar to Coastal Bar Studies in Bo'ao in Eastern Hainan Island of China[J].Marine Geology & Quaternary Geology,2002,22(3):119-127.
[23] 张振克,陈云增,丁海燕,等.海南岛万泉河口地区的海岸侵蚀与灾害风险分析[J].应用基础与工程科学学报,2004,12(增):130-132.
ZHANG Zhen-ke,CHEN Yun-zeng,DING Hai-yan,et al.Coastal Erosion and Risk Analysis in the Estuary Region of the Wanquan River,Hainan Island,China[J].Journal of Basic Science and Engineering,2004,12(S):130-132.
[24] 何幼斌,王文广.沉积岩与沉积相[M].2版.北京:石油工业出版社,2017.
HE You-bin,WANG Wen-guang.Sedimentary Rocks and Facies[M].2nd ed.Beijing:Petroleum Industry Press,2017.
[25] 董大忠,邱 振,张磊夫,等.海陆过渡相页岩气层系沉积研究进展与页岩气新发现[J].沉积学报,2021,39(1):29-45.
DONG Da-zhong,QIU Zhen,ZHANG Lei-fu,et al.Progress on Sedimentology of Transitional Facies Shales and New Discoveries of Shale Gas[J].Acta Se-dimentologica Sinica,2021,39(1):29-45.
[26] 游爱华,薛积彬,谢露华,等.海南东部小海潟湖沉积物地球化学特征及对古台风活动的指示[J].湖泊科学,2019,31(6):1758-1769.
YOU Ai-hua,XUE Ji-bin,XIE Lu-hua,et al.Geochemical Characteristics of Sediments in the Xiaohai Lagoon(Eastern Hainan)and Implications for the Paleo-typhoon Activities[J].Journal of Lake Sciences,2019,31(6):1758-1769.
[27] 曾昭璇,曾宪中.海南岛自然地理[M].北京:科学出版社,2005.
ZENG Zhao-xuan,ZENG Xian-zhong.Physical Geo-graphy of Hainan Island[M].Beijing:Science Press,2005.
[28] 杨湘桃.风景地貌学[M].长沙:中南大学出版社,2005.
YANG Xiang-tao.Landscape Geomorphology[M].Changsha:Central South University Press,2005.
[29] 季荣耀,陆永军,左利钦.曹妃甸老龙沟潮汐通道拦门沙演变机制[J].水科学进展,2011,22(5):645-652.
JI Rong-yao,LU Yong-jun,ZUO Li-qin.Mechanism of Outer Delta Evolution of the Laolonggou Tidal Inlet in Caofeidian Sea Area on China's Bohai Bay[J].Advances in Water Science,2011,22(5):645-652.
[30] 帅 菲,肖根如,揭志强.Google Earth在地学研究中的应用[J].东华理工大学学报(自然科学版),2011,34(1):89-93.
SHUAI Fei,XIAO Gen-ru,JIE Zhi-qiang.Faculty of Geomatics Application of Google Earth in Geoscience Research[J].Journal of East China Institute of Technology(Natural Science Edition),2011,34(1):89-93.
[31] 石书缘,胡素云,冯文杰,等.基于Google Earth软件建立曲流河地质知识库[J].沉积学报,2012,30(5):869-878.
SHI Shu-yuan,HU Su-yun,FENG Wen-jie,et al.Building Geological Knowledge Database of Meandering River Based on Google Earth Software[J].Acta Sedimentologica Sinica,2012,30(5):869-878.
[32] 朱筱敏.沉积岩石学[M].4版.北京:石油工业出版社,2019.
ZHU Xiao-min.Sedimentary Petrology[M].4th ed.Beijing:Petroleum Industry Press,2019.

相似文献/References:

[1]赵永刚,王东旭,冯强汉,等.油气田古地貌恢复方法研究进展[J].地球科学与环境学报,2017,39(04):516.
　ZHAO Yong-gang,WANG Dong-xu,FENG Qiang-han,et al.Review on Palaeomorphologic Reconstruction Methods in Oil and Gas Fields[J].Journal of Earth Sciences and Environment,2017,39(03):516.
[2]冯斌,李华,何幼斌,等.深水等深流沉积中记录的米兰科维奇特性——以陕西富平地区上奥陶统赵老峪组为例[J].地球科学与环境学报,2019,41(01):69.
　FENG Bin,LI Hua,HE You-bin,et al.Characteristics of Milankovitch Cycles in Deep Water Contourites—A Case Study of Upper Ordovician Zhaolaoyu Formation in Fuping Area of Shaanxi, China[J].Journal of Earth Sciences and Environment,2019,41(03):69.
[3]施一凡,李 超*,王 平,等.河流砾-砂过渡带位置变化的控制因素及其指示意义[J].地球科学与环境学报,2023,45(01):54.[doi:10.19814/j.jese.2022.06011]
　SHI Yi-fan,LI Chao*,WANG Ping,et al.Controlling Factors of Migration of Gravel-sand Transition in River Sediment and Its Implications[J].Journal of Earth Sciences and Environment,2023,45(03):54.[doi:10.19814/j.jese.2022.06011]

备注/Memo

备注/Memo:

收稿日期:2022-11-07; 修回日期:2023-01-07
基金项目:国家科技重大专项项目(2016ZX05048)
作者简介:唐明远(1984-),男,四川富顺人,副研究员,E-mail:tangmy.hbsj@sinopec.com。
*通讯作者:赵永刚(1976-),男,甘肃泾川人,教授,工学博士,E-mail:yg_zhao@126.com。

常用功能

更新日期/Last Update: 2023-05-30