Role of gravel in analysis on migration of source area and lake shorelines in lacustrine basin
Gao Zhi-Yong1,2, Shi Yu-Xin1,2, Feng Jia-Rui1,2, Zhou Chuan-Min1,2
1 Petroleum Geology Research and Laboratory Center,PetroChina Research Institute of Petroleum Exploration and Development,Beijing 100083,China; 2 State Key Laboratory of Enhanced Oil Recovery,PetroChina Research Institute of Petroleum Exploration and Development,Beijing 100083,China
Abstract：Low-resolution drilling and seismic imaging in the low-exploration area of the orogenic-basinal regions in the central and western parts of China is complicated. It is difficult to use traditional seismic facies, logging facies or core data to study the palaeogeographic features of the archetypal basin. We established the relationship both between gravel and transport distance, and between gravel development and shoreline migration in the pre-modern alluvial fan, fan delta plain, river and other sedimentary facies. The distance between several outcrops and shorelines from Jurassic to Cretaceous in the Junggar Basin was quantitatively calculated. The evolution process of source area and shorelines of the Junggar Basin in Jurassic to Cretaceous was reconstructed. The palaeogeographic features of the sedimentary archetypes of the basin in the lower-resolution exploration area of the southern and other regions are predicted to provide the basis for predicting the distribution range of the favorable reservoir. The establishment of the delineation of the source area and the quantitative evaluation parameters of the shorelines migration are an important and beneficial supplement for the innovation of traditional sedimentology.
Gao Zhi-Yong,Shi Yu-Xin,Feng Jia-Rui et al. Role of gravel in analysis on migration of source area and lake shorelines in lacustrine basin[J]. JOPC, 2021, 23(3): 507-524.
[1] 程成,任鑫鑫,王微,吕靖文,章媛媛,李双应. 2012. 野外露头砾石圆度测量方法的探究: 以巢湖二叠系栖霞组为例. 沉积学报, 30(3): 522-529. [Cheng C,Ren X X,Wang W,Lü J W,Zhang Y Y,Li S Y.2012. An approach to get gravel roundness data on field outcrops: taking Permian Qixia formation in Chaohu,Anhui Province as an example. Acta Sedimentologica Sinica, 30(3): 522-529] [2] 邓胜徽,卢远征,樊茹,泮燕红,程显胜,付国斌,王启飞,潘华璋,沈炎彬,王亚琼,张海春,贾程凯,段文哲,方琳浩. 2010. 新疆北部的侏罗系. 合肥: 中国科学技术大学出版社. [Deng S H,Lu Y Z,Fan R,Pan Y H,Cheng X S,Fu G B,Wang Q F,Pan H Z,Shen Y B,Wang Y Q,Zhang H C,Jia C K,Duan W Z,Fang L H.2010. The Jurassic System of Northern Xinjiang,China. Hefei: University of Science and Technology of China Press] [3] 邓胜徽,姚益民,叶得泉,陈丕基,金帆,张义杰,许坤,赵应成,袁效奇,张师本. 2003. 中国北方侏罗系(Ⅰ)地层总述. 北京: 石油工业出版社. [Deng S H,Yao Y M,Ye D Q,Chen P J,Jin F,Zhang Y J,Xu K,Zhao Y C,Yuan X Q,Zhang S B.2003. Jurassic System in the North of China,Volume Ⅰ,Stratum Introduction. Beijing: Petroleum Industry Press] [4] 方世虎,贾承造,宋岩,徐怀民,刘楼军. 2005. 准南前陆盆地燕山期构造活动及其成藏意义. 地学前缘, 12(3): 67-76. [Fang S H,Jia C Z,Song Y,Xu H M,Liu L J.2005. The tectonism during Yanshan Period in southern Junggar foreland basin and its implications for hydrocarbon accumulation. Earth Science Frontiers, 12(3): 67-76] [5] 房亚男,吴朝东,王熠哲,马健,周天琪. 2016. 准噶尔盆地南缘中—下侏罗统浅水三角洲类型及其构造和气候指示意义. 中国科学: 技术科学, 46(7): 737-756. [Fang Y N,Wu C D,Wang Y Z,Ma J,Zhou T Q.2016. Lower to Middle Jurassic shallow-water delta types in the southern Junggar Basin and implications for the tectonic and climate(in Chinese). Scientia Sinica-Technologica, 46(7): 737-756] [6] 高志勇,朱如凯,冯佳睿,李小陪,赵雪松,郭美丽. 2015. 库车坳陷侏罗系—新近系砾岩特征变化及其对天山隆升的响应. 石油与天然气地质, 36(4): 534-544. [Gao Z Y,Zhu R K,Feng J R,Li X P,Zhao X S,Guo M L.2015. Relationship between conglomeratic characteristics of Jurassic-Neogene and tectonic uplifting of Tianshan Mountains in Kuqa Depression. Oil and Gas Geology, 36(4): 534-544] [7] 高志勇,周川闽,冯佳睿,吴昊,李雯. 2016a. 中新生代天山隆升及其南北盆地分异与沉积环境演化. 沉积学报, 34(3): 415-435. [Gao Z Y,Zhou C M,Feng J R,Wu H,Li W.2016a. Relationship between the Tianshan Mountains Uplift and depositional environment evolution of the basins in Mesozoic-Cenozoic. Acta Sedimentologica Sinica, 34(3): 415-435] [8] 高志勇,朱如凯,冯佳睿,郑荣才,纪友亮,曾联波,林畅松,周川闽,崔京钢,刘景彦. 2016b. 中国前陆盆地构造-沉积充填响应与深层储层特征. 北京: 地质出版社,1-252. [Gao Z Y,Zhu R K,Feng J R,Zheng R C,Ji Y L,Zeng L B,Lin C S,Zhou C M,Cui J G,Liu J Y.2016b. The Response of Depsition within Tectonic Sequence and Characteristics of Deep Reservoir of Foreland Basin in China. Beijing: Geological Publishing House,1-252] [9] 高志勇,石雨昕,周川闽,冯佳睿,翟羿程,樊小容. 2019a. 砾石分析在扇三角洲与湖岸线演化关系中的应用: 以准噶尔盆地玛湖凹陷周缘百口泉组为例. 沉积学报, 37(3): 550-564. [Gao Z Y,Shi Y X,Zhou C M,Feng J R,Zhai Y C,Fan X R.2019a. The role of gravel in analyzing on the relationship between fan deltas and lake shorelines in a lacustrine basin: case study of the Baikouquan formation around the Mahu depression in Xinjiang. Acta Sedimentologica Sinica,37(3): 550-564] [10] 高志勇,石雨昕,冯佳睿,周川闽,翟羿程,樊小容. 2019b. 水系与构造复合作用下的冲积扇沉积演化: 以南天山山前黄水沟冲积扇为例. 新疆石油地质, 40(6): 638-648. [Gao Z Y,Shi Y X,Feng J R,Zhou C M,Zhai Y C,Fan X R.2019b. Sedimentary evolution of alluvial fan under combined action of drainage system and structure: a case of Huangshuigou alluvial fan in piedmont of Southern Tianshan Mountains. Xinjiang Petroleum Geology, 40(6): 638-648] [11] 管树巍,李本亮,何登发,汪新,John Suppe,雷刚林. 2007. 晚新生代以来天山南、北麓冲断作用的定量分析. 地质学报, 81(6): 725-744. [Guan S W,Li B L,He D F,Wang X,John S,Lei G L.2007. Late Cenozoic active fold-and-thrust belts in the southern and northern flanks of Tianshan. Acta Geologica Sinica, 81(6): 725-744] [12] 管树巍,陈竹新,方世虎. 2012. 准噶尔盆地南缘油气勘探的3个潜在领域: 来自构造模型的论证. 石油勘探与开发, 39(1): 37-44. [Guan S W,Chen Z X,Fang S H.2012. Three potential exploration areas of Southern Junggar Basin: arguments from structural modeling. Petroleum Exploration and Development, 39(1): 37-44] [13] 何开华. 1988. 拜城县卡普沙良下白垩统亚格列木组下段冲积扇的沉积特征. 新疆地质, 6(1): 31-47. [He K H.1988. Sedimentary characteristics of alluvial fans in lower member of Yageliem Formation(Lower Cretaceous),Kapusalion,Baicheng. Xinjiang Geology, 6(1): 31-47] [14] 纪友亮,冯建辉,王声朗,张宏安,王德仁. 2005. 东濮凹陷古近系沙河街组沙三段沉积期湖岸线的变化及岩相古地理特征. 古地理学报, 7(2): 145-156. [Ji Y L,Feng J H,Wang S L,Zhang H A,Wang D R.2005. Shifting of lake shoreline and lithofacies palaeogeographic characters during sedimentary period of the Member 3 of Shahejie Formation of Paleogene in Dongpu Sag. Journal of Palaeogeography(Chinese Edition), 7(2): 145-156] [15] 姜在兴,刘晖. 2010. 古湖岸线的识别及其对砂体和油气的控制. 古地理学报, 12(5): 589-598. [Jiang Z X,Liu H.2010. Lacustrine palaeoshoreline and its controls on sandbodies and hydrocarbon. Journal of Palaeogeography(Chinese Edition), 12(5): 589-598] [16] 况军,邵雨,于兴河. 2014. 准噶尔盆地南缘侏罗系地质剖面图集. 北京: 石油工业出版社,1-202. [Kuang J,Shao Y,Yu X H.2014. Geological Atlas of Jurassic Sections in Southern Junggar Basin. Beijing: Petroleum Industry Press, 1-202] [17] 李本亮,陈竹新,雷永良,张朝军. 2011. 天山南缘与北缘前陆冲断带构造地质特征对比及油气勘探建议. 石油学报, 32(3): 395-403. [Li B L,Chen Z X,Lei Y L,Zhang C J.2011. Structural geology correlation of foreland thrust-folded belts between the southern and northern edges of the Tianshan Mountain and some suggestions for hydrocarbon exploration. Acta Petrolei Sinica, 32(3): 395-403] [18] 李小陪,高志勇,李书凯,冯佳睿,赵雪松,郭美丽. 2013. 库车前陆盆地上侏罗统—下白垩统砾岩特征与构造演化关系. 沉积学报,31(6): 980-993. [Li X P,Gao Z Y,Li S K,Feng J R,Zhao X S,Guo M L.2013. Relationship between conglomeratic characteristics and tectonic evolution of upper Jurassic-lower Cretaceous in Kuqa Foreland Basin. Acta Sedimentologica Sinica, 31(6): 980-993] [19] 李应运,方邺森. 1963. 南京雨花台砾石层的岩组—岩相分析. 南京大学学报(地质学), 3(1): 123-134. [Li Y Y,Fang Y S.1963. Petrofabric lithofacies analysis of gravel bed in Yuhuatai,Nanjing. Journal of Nanjing University(Geology), 3(1): 123-134] [20] 李忠,王道轩,林伟,王清晨. 2004. 库车坳陷中一新生界碎屑组分对物源类型及其构造属性的指示. 岩石学报, 20(3): 655-666. [Li Z,Wang D X,Lin W,Wang Q C.2004. Mesozoic-Cenozoic clastic composition in Kuqa depression,northwest China: implication for provenance types and tectonic attributes. Acta Petrologica Sinica, 20(3): 655-666] [21] 李忠权,陈更生,张寿庭. 1998. 新疆准噶尔盆地南缘拉张伸展动力学环境的探讨. 高校地质学报, 4(1): 73-78. [Li Z Q,Chen G S,Zhang S T.1998. Discussion on the extensional dynamic setting in the south border of Junggar Basin,Xinjiang,China. Geological Journal of China Universities, 4(1): 73-78] [22] 林秀斌,陈汉林,Karl Heinz Wyrwoll,程晓敢,王旭龙,付可昂,廖林,肖骏,Bryan Krapez.2009. 青藏高原东北部隆升: 来自宁夏同心小洪沟剖面的证据. 地质学报, 83(4): 455-467. [Lin X B,Chen H L,Karl Heinz Wyrwoll,Chen X G,Wang X L,Fu K A,Liao L,Xiao J,Bryan Krapez.2009. Uplift of the Northeastern Tibetan Plateau: evidences from the Xiaohonggou Section in Tongxin,Ningxia. Acta Geologica Sinica, 83(4): 455-467] [23] 林潼,王东良,王岚,沈英. 2013. 准噶尔盆地南缘侏罗系齐古组物源特征及其对储层发育的影响. 中国地质, 40(3): 909-918. [Lin T,Wang D L,Wang L,Shen Y.2013. The provenance feature of Jurassic Qigu Formation and its effect on reservoir development in the southern margin of Junggar Basin. Geology in China, 40(3): 909-918] [24] 刘宝珺,曾允孚. 1984. 岩相古地理基础和工作方法. 北京: 地质出版社,1-442. [Liu B J,Zeng Y F.1984. Lithofacies Palaeogeography and Working Method. Beijing: Geological Publishing House,1-442] [25] 刘启亮,刘良刚,何珍,刘启伟,李士涛,朱俊强. 2011. 鄂尔多斯盆地冯地坑—洪德长8油层组湖岸线确定. 海洋地质前沿, 27(4): 38-44. [Liu Q L,Liu L G,He Z,Liu Q W,Li S T,Zhu J Q.2011. Determination of lake shoreline for Chang-8 oil formation in Fengdikeng-Hongde region of Ordos Basin. Marine Geology Frontiers, 27(4): 38-44] [26] 卢远征,邓胜徽. 2009. 准噶尔盆地南缘三叠纪—侏罗纪之交的古气候. 古地理学报, 11(6): 652-660. [Lu Y Z,Deng S H.2009. Palaeoclimate around the Triassic-Jurassic boundary in southern margin of Junggar Basin. Journal of Palaeogeography(Chinese Edition), 11(6): 652-660] [27] 裘善文,万恩璞,江佩芳. 1988. 兴凯湖湖岸线的变迁及松阿察河古河源的发现. 科学通报, (12): 937-940. [Qiu S W,Wan E P,Jiang P F.1988. The changes of the Xingkai lake shoreline and the discovery of Songacha ancient river source. Chinese Science Bulletin, (12): 937-940] [28] 石雨昕,高志勇,周川闽,周正龙. 2017. 新疆焉耆盆地开都河不同河型段砂砾质沉积特征与差异分析. 古地理学报, 19(6): 1037-1048. [Shi Y X,Gao Z Y,Zhou C M,Zhou Z L.2017. Depositional characteristics and variations of different channel deposits in the Kaidu river of Yanqi Basin,Xinjiang. Journal of Palaeogeography(Chinese Edition), 19(6): 1037-1048] [29] 石雨昕,高志勇,周川闽,翟羿程,樊小容,冯佳睿. 2019. 新疆博斯腾湖北缘现代冲积扇与扇三角洲平原分支河流体系的沉积特征与意义. 石油学报, 40(5): 542-556. [Shi Y X,Gao Z Y,Zhou C M,Zhai Y C,Fan X R,Feng J R.2019. Sedimentary characteristics and significance of distributive fluvial system of modern alluvial fan and fan delta plain in the northern margin of Bosten lake,Xinjiang. Acta Petrolei Sinica, 40(5): 542-556] [30] 谭程鹏,于兴河,李胜利,李顺利,陈彬滔,单新,王志兴. 2014. 辫状河—曲流河转换模式探讨: 以准噶尔盆地南缘头屯河组露头为例. 沉积学报, 32(3): 450-458. [Tan C P,Yu X H,Li S L,Li S L,Chen B T,Shan X,Wang Z X.2014. Discussion on the model of braided river transform to meandering river: as an example of Toutunhe Formation in southern Junggar Basin. Acta Sedimentologica Sinica, 32(3): 450-458] [31] 唐湘飞,贾为卫,鲁克改,张强. 2018. 准噶尔盆地南缘下白垩统钙质砾岩铀矿化成因及找矿方向. 新疆地质, 36(3): 399-405. [Tang X F,Jia W W,Lu K G,Zhang Q.2018. Uranium mineralization and prospecting direction of Lower Cretaceous calcareous conglomerate in the southern margin of Junggar Basin. Xinjiang Geology, 36(3): 399-405] [32] 万静萍,马立祥,周宗良,张印斋. 1987. 变形盆地沉积相研究中的几个问题. 石油与天然气地质, 8(4): 448-453. [Wan J P,Ma L X,Zhou Z L,Zhang Y Z.1987. Some problems in the study of sedimentary facies of deformed basin. Oil and Gas Geology, 8(4): 448-453] [33] 万静萍,马立祥,周宗良. 1989. 恢复酒西地区白至系变形盆地原始沉积边界的方法探讨. 石油实验地质, 11(3): 245-249. [Wan J P,Ma L X,Zhou Z L.1989. Approach on the method for restoration of original sedimentary boundaries of the Cretaceous deformed basin in Jiuxi area. Experimental Petroleum Geology,11(3): 245-249] [34] 王龙樟. 1994. 准噶尔盆地中新生代湖水位升降曲线的建立与剖析. 岩相古地理, 14(6): 1-14. [Wang L Z.1994. Approaches to the curves for the lake level fluctuations in the Junggar Basin during Meso-Cenozoic time. Sedimentary Facies and Palaeogeography, 14(6): 1-14] [35] 王龙樟. 1995. 准噶尔盆地中新生代陆相层序地层学探讨及其应用. 新疆石油地质, 16(4): 324-330. [Wang L Z.1995. A study on Mesozoic-Cenozoic continental sequence stratigraphy and its application in Junggar Basin. XinJiang Petroleum Geology, 16(4): 324-330] [36] 魏光辉. 2015. 气候变化对新疆黄水沟流域径流过程的影响. 浙江水利水电学院学报, 27(1): 46-57. [Wei G H.2015. Climate change on runoff process in Huangshuigou river basin. Journal of Zhejiang University of Water Research & Electric Power, 27(1): 46-57] [37] 卫平生,潘树新,王建功,雷明. 2007. 湖岸线和岩性地层油气藏的关系研究: 论“坳陷盆地湖岸线控油”.岩性油气藏, 19(1): 27-31. [Wei P S,Pan S X,Wang J G,Lei M.2007. Study of the relationship between lithostratigraphic reservoirs and lakeshore line: introduction on lakeshore line controlling oil/gas reservoirs in sag basin. Lithologic Reservoirs, 19(1): 27-31] [38] 吴磊伯. 1957. 砾石定向测量的意义与方法. 地质知识, 12: 1-6. [Wu L B.1957. Significance and method of gravel orientation survey. Geological Knowledge, 12: 1-6] [39] 吴磊伯,马胜云,沈淑敏. 1958. 砾石排列方位的分析并论述长沙等地白沙井砾石层的沉积构造. 地质学报, 38(2): 201-231. [Wu L B,Ma S Y,Shen S M.1958. Analysis of gravel arrangement orientation and discussion on sedimentary structure of baishajing gravel layer in Changsha and other places. Acta Geologica Sinica, 38(2): 201-231] [40] 吴磊伯,沈淑敏. 1962. 海滨砾石粗构分析的一个实例. 地质学报, 42(4): 353-361. [Wu L B,Shen S M.1962. An example of fabric analysis of beach gravels. Acta Geologica Sinica, 42(4): 353-361] [41] 吴锡浩,钱方. 1964. 川江徐家沱—金刚沱河段现代河床砾石粒度和形态变化的初步分析. 地质论评, 22(4): 289-297. [Wu X H,Qian F.1964. Preliminary analysis of grain size and morphological changes of the modern river bed gravel in the lower reaches of the Chuanjiang River,Sichuan Province. Geological Review, 22(4): 289-297] [42] 薛刚. 2011. 乌什塔拉河水文特性分析. 水利科技与经济, 17(8): 17-19. [Xue G.2011. The hydrological characteristics analysis of Wushitala river. Water Conservancy Science and Technology and Economy, 17(8): 17-19] [43] 杨克文,庞军刚,李文厚. 2009. 坳陷湖盆湖岸线的确定方法: 以志丹地区延长组为例. 兰州大学学报(自然科学版), 45(3): 13-17. [Yang K W,Pang J G,Li W H.2009. Determination method of lake shoreline in depressed-type lacustrine basin: taking the Yanchang formation of Zhidan area as an example. Journal of Lanzhou University(Natural Sciences), 45(3): 13-17] [44] 余素玉. 1984. 砾岩和角砾岩的组分—成因分类. 地质科技情报,(3): 37-40. [Yu S Y.1984. Components of conglomerate and breccia-genetic classification. Geological Information Science and Technology,(3): 37-40] [45] 曾宜君,杨学俊,李云泉,谢启兴,朱兵,郝雪峰. 2004. 川西前陆盆地南部中新生代砾岩的构造意义. 四川地质学报, 24(4): 198-201. [Zeng Y J,Yang X J,Li Y Q,Xie Q X,Zhu B,Hao X F.2004. Tectonic significance of Meso-Cenozoic conglomerate in the south of the West Sichuan Foreland Basin. Sichuan Journal of Geology, 24(4): 198-201] [46] 张庆云,田德利. 1986. 利用砾石形状和圆度判别第四纪堆积物的成因. 长春地质学院学报,(1): 59-64. [Zhang Q Y,Tian D L.1986. The identification of the origin of quaternary accumulative material by shape and roundness of gravels. Journal of Changchun College of Geology,(1): 59-64] [47] 周天琪,吴朝东,袁波,史忠奎,王家林,朱文,周彦希,姜晰,赵进雍,王军,马健. 2019. 准噶尔盆地南缘侏罗系重矿物特征及其物源指示意义. 石油勘探与开发, 46(1): 65-78. [Zhou T Q,Wu C D,Yuan B,Shi Z K,Wang J L,Zhu W,Zhou Y X,Jiang X,Zhao J Y,Wang J,Ma J.2019. New insights into multiple provenances evolution of the Jurassic from heavy minerals characteristics in southern Junggar Basin,NW China. Petroleum Exploration and Development, 46(1): 65-78] [48] 朱大岗,赵希涛,孟宪刚,吴中海,邵兆刚,冯向阳,王津,杨朝斌. 2002. 念青唐古拉山主峰地区第四纪砾石层砾组分析. 地质力学学报, 8(4): 323-332. [Zhu D G,Zhao X T,Meng X G,Wu Z H,Shao Z G,Feng X Y,Wang J,Yang C B.2002. Fabric analysis of gravel in quternary gravel beds on backbone area of Nianqingtagulashan Mountain. Journal of Geomechanics, 8(4): 323-332] [49] Alexander C W,Robert A D,Joshua S,Rosie A S,Amy L W,Philip A A.2011. Decoding downstream trends in stratigraphic grain size as a function of tectonic subsidence and sediment supply. Geological Society of America Bulletin,123(7/8): 1363-1382. doi: 10.1130/B30351.1. [50] Cornel O,Janok P B.2006. Terminal distributary channels and delta front architecture of river-dominated delta systems. Journal of Sedimentary Research, 76: 212-233. [51] Gale S J,Ibrahim Z Z,Lal J,Sicinilawa U B T.2019. Downstream fining in a megaclast-dominated fluvial system: the Sabeto river of western Viti Levu,Fiji. Geomorphology, 330: 151-162. [52] Gao Z Y,Guo H L,Zhu R K,Zhang L J,Sun Y S.2009. Sedimentary response of different fan types to the Paleogene-Neogene basin transformation in the Kuqa Depression,Xinjiang. Acta Geologica Sonica(English Edition), 83(2): 411-424. [53] Hoey T B, Bluck B J.1999. Identifying the controls over downstream fi ning of river gravels. Journal of Sedimentary Research, 69: 40-50. [54] Michael B S.2008. Downstream patterns of bed material grain size in a large,lowland alluvial river subject to low sediment supply. Water Resources Research, 44: W12202,1-7. doi: 10.1029/2008WR007183. [55] Nicola S.2002. Downstream variation in grain size along an Alpine river: analysis of controls and processes. Geomorphology, 43: 137-149. [56] Paola C,Heller P,Angevine C.1992a. The largescale dynamics of grain size variation in alluvial basins: 1. Theory. Basin Research, 4: 73-90. [57] Paola C,Parker G,Seal R,Shina S K,Southard J B,Wilcock P R.1992b. Downstream fining by selective deposition in a laboratory flume. Science, 258: 1757-1760. doi: 10.1126/science.258.5089.1757. [58] Robinson R A J,Slingerland R L.1998. Grain size trends,basin subsidence and sediment supply in the Campanian Castlegate Sandstone,and equivalent conglomerates of central Utah. Basin Research, 10: 109-127. doi: 10.1046/j.1365-2117.1998.00062.x.
