LATE MESOZOIC DEPOSITS AND THEIR CHARACTERISTICS OF RIQINGWEI BASIN IN THE NEARSHORE AREA OF EASTERN SHANDONG

LIU Feifei; ZHOU Yaoqi; ZHANG Zhenkai; LI Manjie; GU Yangjian; SHAN Jiaqi; ZHOU Tengfei

doi:10.16028/j.1009-2722.2020.162

2021 Vol. 37, No. 3

Article Contents

Article navigation > Marine Geology Frontiers > 2021 > 37(3): 22-32

Next Article Previous Article

LIU Feifei, ZHOU Yaoqi, ZHANG Zhenkai, LI Manjie, GU Yangjian, SHAN Jiaqi, ZHOU Tengfei. LATE MESOZOIC DEPOSITS AND THEIR CHARACTERISTICS OF RIQINGWEI BASIN IN THE NEARSHORE AREA OF EASTERN SHANDONG[J]. Marine Geology Frontiers, 2021, 37(3): 22-32. doi: 10.16028/j.1009-2722.2020.162

Citation:

LIU Feifei, ZHOU Yaoqi, ZHANG Zhenkai, LI Manjie, GU Yangjian, SHAN Jiaqi, ZHOU Tengfei. LATE MESOZOIC DEPOSITS AND THEIR CHARACTERISTICS OF RIQINGWEI BASIN IN THE NEARSHORE AREA OF EASTERN SHANDONG[J]. Marine Geology Frontiers, 2021, 37(3): 22-32. doi: 10.16028/j.1009-2722.2020.162

LATE MESOZOIC DEPOSITS AND THEIR CHARACTERISTICS OF RIQINGWEI BASIN IN THE NEARSHORE AREA OF EASTERN SHANDONG

1.
School of Architectural Engineering, Binzhou University, Binzhou 256600, Shandong, China
2.
School of Geosciences, China University of Petroleum (East China), Qingdao 266580, China
3.
Shaanxi Institute of Geological Survey, Xi'an 710054, China
4.
Shandong Institute of Geophysical and Geochemical Exploration, Jinan 250013, China
5.
Jinneng Science and Technology Company Limited, Qingdao 266000, China

More Information

Corresponding author: ZHOU Yaoqi, zhouyq@upc.edu.cn

Received Date: 16 October 2020

Publish Date: 28 March 2021

Abstract

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.
- nearshore area of Eastern Shandong /
- Late Mesozoic /
- stratigraphy /
- sedimentary characteristics

FullText(HTML)

References

[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. Google Scholar
[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 CrossRef Google Scholar
[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. Google Scholar
[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 CrossRef Google Scholar
[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 CrossRef Google Scholar
[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. Google Scholar
[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 CrossRef Google Scholar
[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 CrossRef Google Scholar
[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 CrossRef Google Scholar
[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. Google Scholar
[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 CrossRef Google Scholar
[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 CrossRef Google Scholar
[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 CrossRef Google Scholar
[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. Google Scholar
[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 CrossRef Google Scholar
[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 CrossRef Google Scholar
[17]	蔡乾忠. 中国海域油气地质学[M]. 北京: 海洋出版社, 2005: 77-92. Google Scholar
[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. Google Scholar
[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 CrossRef Google Scholar
[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 CrossRef Google Scholar
[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. Google Scholar
[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 CrossRef Google Scholar
[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. Google Scholar
[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 CrossRef Google Scholar
[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 CrossRef Google Scholar
[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. Google Scholar
[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. Google Scholar
[28]	BOUMA A H. Sedimentology of some flysh deposits: a graphic approach to facies interpretation[M]. Amasterdam: Elsevier Publishing Company, 1962: 168. Google Scholar