LATE MESOZOIC DEPOSITS AND THEIR CHARACTERISTICS OF RIQINGWEI BASIN IN THE NEARSHORE AREA OF EASTERN SHANDONG
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摘要:
山东东部近海地区出露的晚中生代深水沉积受到地质学界越来越多的关注。但目前，关于晚中生代地层沉积充填特征还未有过系统细致的研究。选取出露于青岛灵山岛、崂山、诸城桃林、海阳丁字湾、即墨周戈庄等山东东部近海地区的5个典型剖面，开展了详细的地层沉积特征研究。晚中生代地层主要为莱阳群和青山群沉积，莱阳群岩性以深水重力流沉积岩和硅质碎屑岩为特征；青山群岩性以火山碎屑岩为特征。总体上，莱阳群到青山群自下而上为海进—海退过程。
Abstract:Late Mesozoic deep-water sediments occur widely in the area off Eastern Shandong Peninsula, which have received great attention from geologists recently. However, the research on Late Mesozoic and its sedimentary characteristics of the area has not been systematically conducted in details so far. In this paper, the five field typical profiles at the Lingshan Island, Laoshan, Taolin, Dingzi Bay and Zhougezhuang areas are selected for detailed case studies. The Late Mesozoic includes the Laiyang and Qingshan Groups. The Laiyang Group is characterized by gravity flow and siliceous clastic deposits, and the Qingshan Group is characterized by pyroclastic rocks. From the Laiyang Group to the Qingshan Group it is a transgression-regression cycle.
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[1] WU F Y,LIN J Q,WILDE S A,et al. Nature and significance of the Early Cretaceous giant igneous event in Eastern China[J]. Earth and Planetary Science Letters,2005,233(1):103-119.
[2] 孙卫东,凌明星,汪方跃,等. 太平洋板块俯冲与中国东部中生代地质事件[J]. 矿物岩石地球化学通报,2008,27(3):218-225. doi: 10.3969/j.issn.1007-2802.2008.03.002
[3] 李三忠,郑祺亮,李玺瑶,等. 中国东部苏鲁造山带的印支期俯冲极性及其造山过程[J]. 海洋地质与第四纪地质,2017,37(4):18-32.
[4] 吴智平,侯旭波,李伟. 华北东部地区中生代盆地格局及演化过程探讨[J]. 大地构造与成矿学,2007,31(4):385-399. doi: 10.3969/j.issn.1001-1552.2007.04.001
[5] 张岳桥,赵越,董树文,等. 中国东部及邻区早白垩世裂陷盆地构造演化阶段[J]. 地学前缘,2004,11(3):123-133. doi: 10.3321/j.issn:1005-2321.2004.03.014
[6] 周瑶琪,张振凯,梁文栋,等. 山东东部晚中生代构造-岩浆活动及原型盆地恢复[J]. 地学前缘,2015,22(1):137-156.
[7] 张松梅,程立人,刘典涛. 胶南地区莱阳群绒枝藻化石的发现[J]. 长春科技大学学报,2001,31(3):209-212. doi: 10.3969/j.issn.1671-5888.2001.03.001
[8] 付永涛,虞子冶. 青岛垭口-八仙墩变质海相碎屑岩的属性和构造意义[J]. 地质科学,2010,45(1):207-227. doi: 10.3969/j.issn.0563-5020.2010.01.018
[9] 吴拓宇,赵淑娟,付永涛. 青岛八仙墩海相碎屑岩的岩石地球化学特征及其油气研究意义[J]. 地质科学,2010,45(4):1156-1169. doi: 10.3969/j.issn.0563-5020.2010.04.018
[10] 吕洪波,王俊,张海春. 山东灵山岛晚中生代滑塌沉积层的发现及区域构造意义初探[J]. 地质学报,2011,85(6):938-946.
[11] WANG J,CHANG S C,LU H B,et al. Detrital zircon U-Pb age constraints on Cretaceous sedimentary rocks of Lingshan Island and implications for tectonic evolution of Eastern Shandong,North China[J]. Journal of Asian Earth Sciences,2014,96:27-45. doi: 10.1016/j.jseaes.2014.09.002
[12] WANG J,CHANG S C,LIN P,et al. Evidence of Early Cretaceous transpression in the Sulu orogenic belt,Eastern China[J]. Tectonophysics,2016,687:44-55. doi: 10.1016/j.tecto.2016.09.005
[13] 周瑶琪,辜洋建,周腾飞,等. 山东东部白垩系莱阳群沉积地层与有机质特征[J]. 石油与天然气地质,2019,40(1):109-122. doi: 10.11743/ogg20190111
[14] 张振凯,周瑶琪,彭甜明,等. 山东灵山岛莱阳群粉砂岩地球化学特征及意义[J]. 地球科学,2017,42(3):357-377.
[15] LIU F,ZHOU Y,ZHANG Z,et al. Detrital zircon U-Pb geochronology of Early Cretaceous sedimentary rocks in Dingzi Bay and Taolin area from the Sulu Orogen:provenances and tectonic implications[J]. Geological Journal,2019,54:2693-2715. doi: 10.1002/gj.3364
[16] 李曼洁,周瑶琪,周腾飞,等. 山东即墨地区下白垩统灰岩地球化学特征及沉积环境分析[J]. 地质与资源,2020,29(2):126-134,125. doi: 10.3969/j.issn.1671-1947.2020.02.003
[17] 蔡乾忠. 中国海域油气地质学[M]. 北京: 海洋出版社, 2005: 77-92.
[18] 惠若愚. 苏鲁造山带浅部构造特征及深部动力学过程分析[D]. 青岛: 中国石油大学(华东), 2012.
[19] LIU F,GERDES A,ROBINSON P T,et al. Zoned zircon from eclogitelenses in marbles from the Dabie-Sulu UHP Terrane,China:a clear record of ultra-deep subduction and fast exhumation[J]. Acta Geology Sinica,2007,81:204-225. doi: 10.1111/j.1755-6724.2007.tb00945.x
[20] YANG J S,WOODEN J L,WU C L,et al. SHRIMP U-Pb dating of coesite-bearing zircon from the ultrahigh-pressure metamorphic rocks,Sulu Terrane,East China[J]. Journal of Metamorphic Geology,2003,21(6):551-560. doi: 10.1046/j.1525-1314.2003.00463.x
[21] TANG J,ZHENG Y F,WU Y B,et al. Zircon U-Pb age and geochemical constraints on the tectonic affinity of the Jiaodong Terrane in the Sulu Orogen,China[J]. Precambrian Research,2008,161(3):389-418.
[22] 刘福来,薛怀民. 苏鲁超高压变质带含褐帘石正、副片麻岩中变质锆石的地球化学性质及其SHRIMP U-Pb定年[J]. 岩石学报,2007,23(12):3137-3152. doi: 10.3969/j.issn.1000-0569.2007.12.007
[23] MA L,JIANG S Y,DAI B Z,et al. Multiple sources for the origin of Late Jurassic Linglong Adakitic granite in the Shandong Peninsula,Eastern China:zircon U-Pb geochronological,geochemical and Sr-Nd-Hf isotopic evidence[J]. Lithos,2013,162-163(Complete):251-263.
[24] CHEN F K,GUO J H,JIANG L L,et al. Provenance of the Beihuaiyang lower-grade metamorphic zone of the Dabie ultrahigh pressure collisional orogen,China:evidence from zircon ages[J]. Journal of Asian Earth Sciences,2003,22:343-352. doi: 10.1016/S1367-9120(03)00068-3
[25] 郭敬辉,陈福坤,张晓曼,等. 苏鲁超高压带北部中生代岩浆侵入活动与同碰撞-碰撞后构造过程:锆石 U-Pb 年代学[J]. 岩石学报,2005,21(4):1281-1301. doi: 10.3321/j.issn:1000-0569.2005.04.025
[26] 张娟. 苏鲁造山带中生代岩浆岩地球化学研究[D]. 合肥: 中国科学技术大学, 2011.
[27] 刘菲菲,周瑶琪,许红,等. 灵山岛成因特征、类型及其地质构造意义[J]. 海洋地质前沿,2016,32(3):33-40.
[28] BOUMA A H. Sedimentology of some flysh deposits: a graphic approach to facies interpretation[M]. Amasterdam: Elsevier Publishing Company, 1962: 168.
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