Route Planning and Ponder of Geoscience Study Travel in Hualong County, Qinghai Province

doi:10.19657/j.geoscience.1000-8527.2023.113

Abstract

Abstract:

Geoscience study travel is a new engine to utilize the resources of geological heritage to carry out the popularization of geoscience, which in turn leads to geotourism. Yet, due to the fact that the guiding ideology and methodology of study route planning are still unclear, there are problems such as limited study objects, superficial course contents, insufficient scientific inquiry, and emphasizing on touring but not on studying, etc. in geoscience study in general. Hualong County in Qinghai Province, which is located in the upper reaches of the Yellow River, preserving significant geological heritage such as the convergence of Rodinia supercontinent, the subduction and closure of the Proto-Tethys Ocean, the uplift of the Tibetan Plateau and the Yellow River evolution, etc., which is a unique resource to carry out geoscience study travel. This paper discusses the design ideas of geoscience study planning from the guiding ideology, scientific questions and supporting facilities, taking Huarong County as an example.Based on the detailed field geological survey, the characteristics, types, distribution and scientific value of geological heritage in Hualong County have been systematically researched and deeply excavated. Taking the Early Paleozoic Ophiolite Suite in Laji Mountain, Xining Group-Hualong Complex Angular Unconformity, Danxia landform, Red Soil Forest landform and paleoseismic dammed-lake as the key points of the study, we have planned out the Lamu Gorge-Heshijia “the Meeting of one Billion Years”, Ahetan Village-Gongbo Gorge “Flowing Water-the Sculptor of Nature”, Keba Village-Jinyuan Township “Double-edged Sword of Neotectonic Movement”, Yaoshuiquan-Ansiduo Township “Conversion of Sea and Land with Ophiolite”, Xiaqiong Temple-Gangshan Mountain “the Winding Yellow River, the Forest Sea of Plateau”, a total of five geoscience study routes. It also proposes the methods of planning and designing geoscience study routes oriented by geoscience questions and guided by the earth system view and the theory of harmonious coexistence between man and nature. It can provide a scientific basis for the development of geotourism in Hualong County, and also has a certain reference value for the development of geoscience study in other areas.

Key words: geoscience study travel, geological heritage, route planning, Hualong County, Yellow River, northeastern margin of the Tibetan Plateau

CLC Number:

P931.2

LI Junlei, ZHANG Xujiao, WANG Yifan, ZHANG Xiangge, WANG Chongge, YUAN Xiaoning, LIU Xinlan, WANG Kaiya, RAO Haoshu, LIU Jiang, QIN Yuan. Route Planning and Ponder of Geoscience Study Travel in Hualong County, Qinghai Province[J]. Geoscience, 2023, 37(05): 1411-1422.

Figures/Tables 5

Fig.1 Traffic and topographic map of Hualong County in Qinghai Province

Fig.2 Map showing five Geoscience Study Routes in Hualong County

Fig.3 Main study sites of Geoscience Study Routes ① and ② in Hualong County

Fig.4 Main study sites of Geoscience Study Route ③ in Hualong County

Fig.5 Main study sites of Geoscience Study Route ④ and ⑤ in Hualong County

References 76

[1]	ZHANG X G, ZHANG X J, WANG H. The Principles and Methods of Route Design for Study Travel in Laoheishan Scenic Area of Wudalianchi UNESCO Global Geopark[C] Hubei Zhongke Geology and Environment Technology Institute. Proceedings of the 7th Academic Conference of Geology Resource Management and Sustainable Development. Aussino Academic Publishing House, 2019:977-982.
[2]	段玉山, 袁书琪, 郭锋涛, 等. 研学旅行课程标准(一)——前言、课程性质与定位、课程基本理念、课程目标[J]. 地理教学, 2019(5): 4-7.
[3]	矫炎瑾, 黄悦雯, 马婧妮, 等. 文旅融合背景下地学类研学旅行产品开发探究[J]. 当代旅游, 2021, 19(33):16-18.
[4]	陈安泽. 研学旅行、地学旅游以及疫后旅游之我见[M]// 中国地质科学院. 中国地质学会旅游地学与地质公园研究分会第34届年会暨福建龙岩地质公园建设与旅游发展研讨会论文集. 北京: 中国林业出版社, 2019:18-21.
[5]	RITCHIE B W, CARR N, COOPER C. Managing Educational Tourism[M]. Bristol: Channel View Publications, 2003.
[6]	中国旅游研究院产业研究所研学旅行课题组. 中国研学旅行发展报告2022—2023[R]. 2023.
[7]	董婷婷, 蔡杨, 施珂, 等. 探讨新时代地勘单位如何在研学旅行中发挥重要作用[J]. 世界有色金属, 2019(14): 157-158.
[8]	梁山泉, 潘鑫. 科普研学:张家界旅游的新品牌[N]. 张家界日报, 2023-07-01(2).
[9]	何瑶瑶, 熊平生, 陈婷, 等. 基于4F教学模式的高中自然地理研学旅行课程设计——以张家界世界地质公园为例[J]. 地理教育, 2023(4): 66-69.
[10]	占义勇, 陈留勤, 郭福生, 等. 龙虎山地学研学路线的自然和人文景观[M]//江西地学新进展2020——江西省地质学会第十次会员代表大会暨江西省地质学会2020年学术年会论文集. 南昌: 江西省地质学会, 2020: 167-171.
[11]	石玉颖. 基于地理实践力培养的研学旅行活动设计与实施——以中国克什克腾世界地质公园为例[J]. 科学咨询(科技·管理), 2023(5): 239-242.
[12]	孙国念. 指向地理实践力培养的研学旅行活动设计——以韶关丹霞山研学旅行为例[J]. 中学地理教学参考, 2021(8): 77-79.
[13]	杨佳丽, 姜勇彪. 研学旅行视角下旅游地学文化村的建设探索——以梅岭铜源峡为例[J]. 国土与自然资源研究, 2022(4): 81-83.
[14]	WANG Y X, LI G Q, WANG X Y, et al. Single-grain K-feldspar pIRIR dating of the Shalongka archeological site revealed the relationship between monsoon,overbank flooding, and human occupation during the Holocene on the northeastern Tibetan Plateau[J]. Quaternary Science Reviews, 2022, 298: 107848. DOI URL
[15]	赵珍珍, 肖永明, 郭荣臻, 等. 青海化隆沙隆卡遗址生业经济研究——来自淀粉粒的证据[J]. 考古与文物, 2021(6): 120-125.
[16]	伯果, 谢继胜, 扎西尖措, 等. 青海化隆旦斗岩窟壁画初步调查[J]. 考古与文物, 2014(2): 24-30.
[17]	马敏敏, 董广辉, 贾鑫, 等. 青海省化隆县新石器—青铜时代聚落形态及其影响因素分析[J]. 第四纪研究, 2012, 32(2): 209-218.
[18]	YAN Z, FU C, AITCHISON J C, et al. Retro-foreland basin development in response to Proto-Tethyan Ocean closure, NE Tibet Plateau[J]. Tectonics, 2019, 38: 4229-4248. DOI URL
[19]	YAN Z, AITCHISON J, FU C L, et al. Hualong Complex, South Qilian terrane: U-Pb and Lu-Hf constraints on Neoproterozoic micro-continental fragments accreted to the northern Proto-Tethyan margin[J]. Precambrian Research, 2015, 266: 65-85. DOI URL
[20]	WANG T, WANG Z, YAN Z, et al. Geochronological and geochemical evidence of amphibolite from the Hualong Group, northwest China: Implication for the Early Paleozoic accretionary tectonics of the Central Qilian belt[J]. Lithos, 2016, 248-251: 12-21.
[21]	LEASE R O, BURBANK D W, HOUGH B, et al. Pulsed Miocene range growth in northeastern Tibet: Insights from Xunhua Basin magnetostratigraphy and provenance[J]. Geological Society of America Bulletin, 2012, 124(5/6): 657-677. DOI URL
[22]	徐旺春, 张宏飞, 柳小明. 锆石U-Pb定年限制祁连山高级变质岩系的形成时代及其构造意义[J]. 科学通报, 2007, 53(10): 1174-1180.
[23]	闫臻, 牛漫兰, 付长垒, 等. 拉脊山昂思多蛇绿岩-增生杂岩1∶25000专题地质图数据集[J]. 中国地质, 2021, 48(1): 53-65.
[24]	张远泽, 王国灿, 王岸, 等. 循化—化隆盆地晚白垩世以来盆山耦合过程:来自物源与磷灰石裂变径迹年代学分析的证据[J]. 地球科学(中国地质大学学报), 2013, 38(4): 725-744.
[25]	袁道阳, 张培震, 方小敏, 等. 青藏高原东北缘临夏盆地晚新生代构造变形及过程[J]. 地学前缘, 2007, 14(1): 243-250.
[26]	张照伟, 李文渊, 王亚磊, 等. 南祁连化隆地区下什堂含铜镍矿基性-超基性岩体成因研究:锆石年代学、地球化学和Sr-Nd同位素约束[J]. 岩石学报, 2015, 31(9): 2539-2548.
[27]	李文渊. 祁连山岩浆作用有关硫化金属矿床成矿与找矿[D]. 西安: 西北大学, 2006.
[28]	张照伟. 南祁连化隆地区镁铁—超镁铁质侵入岩地质、地球化学特征与铜镍成矿[D]. 西安: 长安大学, 2013.
[29]	GUO X H, FORMAN S L, MARIN L, et al. Assessing tectonic and climatic controls for Late Quaternary fluvial terraces in Guide, Jianzha, and Xunhua Basins along the Yellow River on the northeastern Tibetan Plateau[J]. Quaternary Science Reviews, 2018, 195: 109-121. DOI URL
[30]	潘保田, 李吉均, 曹继秀, 等. 化隆盆地地貌演化与黄河发育研究[J]. 山地研究, 1996(3): 153-158.
[31]	WU Q L, ZHAO Z J, LIU L, et al. Outburst flood at 1920 BCE supports historicity of China’s Great Flood and the Xia dynasty[J]. Science, 2016, 353: 579-582. DOI URL
[32]	ZHANG Y Z, HUANG C C, JAMES S, et al. Formation and evolution of the Holocene massive landslide-dammed lakes in the Jishixia Gorges along the upper Yellow River: No relation to China’s Great Flood and the Xia Dynasty[J]. Quaternary Science Reviews, 2019, 218: 267-280. DOI URL
[33]	HUANG Y, XU C, LI L, et al. Inventory and spatial distribution of ancient landslides in Hualong County, China[J]. Land, 2023, 12(1): 136. DOI URL
[34]	魏刚, 殷志强, 史立群, 等. 青海化隆县地质灾害易发性区划[J]. 中国地质灾害与防治学报, 2013, 24(1): 86-92.
[35]	黄河流域生态保护和高质量发展规划纲要[N]. 人民日报, 2021-10-09(1).
[36]	卓玛措, 卜诗洁. 青海省构建国际生态旅游目的地:系统分析与路径选择[J]. 青海民族研究, 2022, 33(3):40-45.
[37]	袁道阳, 张培震, 雷中生, 等. 青海拉脊山断裂带新活动特征的初步研究[J]. 中国地震, 2005(1): 93-102.
[38]	张波. 西秦岭北缘断裂西段与拉脊山断裂新活动特征研究[D]. 北京: 中国地震局兰州地震研究所, 2012.
[39]	李智敏, 李延京, 田勤俭, 等. 拉脊山断裂古地震与喇家遗址灾变事件关系研究[J]. 地震研究, 2014, 37(1): 109-115.
[40]	LI Y L, TONG X, ZHU Y H, et al. Tectonic affinity and evolution of the Precambrian Qilian block: Insights from petrology, geochemistry and geochronology of the Hualong Group in the Qilian Orogen, NW China[J]. Precambrian Research, 2018, 315: 179-200. DOI URL
[41]	FU C L, YAN Z, AITCHISON J C, et al. Relicts of a Cambrian oceanic arc in the Lajishan suture, NE Tibetan Plateau: Evidence for early-stage subduction within the Proto-Tethyan Ocean[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2022, 585:110713. DOI URL
[42]	FU CL, YAN Z, WANG Z Q. Lajishankou ophiolite complex: implications for Paleozoic multiple accretionary and collisional events in the South Qilian Belt[J]. Tectonics, 2018, 37:1321-1346. DOI URL
[43]	YAN Z, FU C L, AITCHISON J C, et al. Arc-continent collision during culmination of Proto-Tethyan Ocean closure in the Central Qilian belt, NE Tibetan Plateau[J]. Geological Society of America Bulletin, 2022, 134(11/12): 3079-3098. DOI URL
[44]	付长垒, 闫臻, 王秉璋, 等. 造山带中古海山残片的识别——以拉脊山缝合带青沙山和东沟地质填图为例[J]. 地质通报, 2021, 40(1): 31-40.
[45]	LIU S H, ZHANG G W, PAN F, et al. Timing of Xunhua and Guide basin development and growth of the northeastern Tibetan Plateau, China[J]. Basin Research, 2013, 25(1): 74-96. DOI URL
[46]	HE C C, ZHANG Y Q, LI S K, et al. Magnetostratigraphic study of a Late Cretaceous-Paleogene succession in the eastern Xining basin, NE Tibet: Constraint on the timing of major tectonic events in response to the India-Eurasia collision[J]. GSA Bulletin, 2021, 133(11/12): 2457-2484. DOI URL
[47]	FANG X M, FANG Y H, ZAN J B, et al. Cenozoic magnetostratigraphy of the Xining Basin, NE Tibetan Plateau, and its constraints on paleontological, sedimentological and tectonomorphological evolution[J]. Earth-Science Reviews, 2019, 190: 460-485. DOI URL
[48]	王重歌, 李俊磊, 张绪教, 等. 拟建的青海化隆国家地质公园地质遗迹特征及评价[J]. 现代地质, 2023, 37(2): 512-528.
[49]	刘心兰, 张绪教, 李俊磊, 等. 青海化隆县独特的峡谷丹山地貌景观及其科学价值[J]. 现代地质, 2023, 37(1): 233-244.
[50]	孙鸣生, 王国道. 青海化隆、循化两县考古调查简报[J]. 考古, 1991(4): 313-331.
[51]	贾鑫. 青海省东北部地区新石器——青铜时代文化演化过程与植物遗存研究[D]. 兰州: 兰州大学, 2012.
[52]	陆离. 关于青海化隆丹斗地区佛教遗迹的几个问题[J]. 西藏民族大学学报(哲学社会科学版), 2021, 42(3): 37-43+85+154.
[53]	卓玛吉. 论夏琼寺的宗教地位及文化价值[D]. 北京: 中央民族大学, 2011.
[54]	GAO J Y, HOU G L, XIAO Y M, et al. Vegetation history and survival patterns of the earliest village on the Qinghai-Tibetan Plateau[J]. Frontiers in Plant Science, 2022, 13: 903192. DOI URL
[55]	LI G Q, DONG G H, WEN L J, et al. Overbank flooding and human occupation of the Shalongka site in the Upper Yellow River Valley, northeast Tibet Plateau in relation to climate change since the last deglaciation[J]. Quaternary Research, 2014, 82(2): 354-365. DOI URL
[56]	王宗礼, 曹辉辉, 肖永明, 等. 青藏高原东北部沙隆卡遗址史前人群活动和生存环境基础[J]. 第四纪研究, 2021, 41(1): 201-213.
[57]	肖永明. 青海化隆伊沙尔河口史前遗址的学术价值[J]. 青海师范大学学报(哲学社会科学版), 2013, 35(6): 49-52.
[58]	肖永明. 青海东部地区仰韶文化的发展阶段探析[J]. 青海民族大学学报(社会科学版), 2013, 39(4): 58-62.
[59]	刘东生. 走向“地球系统”的科学:地球系统科学的学科雏形及我们的机遇[J]. 中国科学基金, 2006(5): 266-271.
[60]	“中国学科及前沿领域发展战略研究(2021—2035)”项目组. 中国地球科学2035发展战略[M]. 北京: 科学出版社,2023.
[61]	中国科学院地学部“中国地球科学发展战略”研究组. 地球科学: 世纪之交的回顾与展望[M]. 青岛: 山东教育出版社, 2002.
[62]	汪品先. 我国的地球系统科学研究向何处去[J]. 地球科学进展, 2003, 18(6): 837-851. DOI
[63]	汪品先. 地球系统与演变[M]. 北京: 科学出版社, 2018.
[64]	孙继敏. 地球系统科学的研究范例—青藏高原隆升的地貌、环境、气候效应[J]. 中山大学学报(自然科学版), 2014, 53(6): 1-9.
[65]	李三忠, 刘丽军, 索艳慧, 等. 碳构造:一个地球系统科学新范式[J]. 科学通报, 2023, 68(4): 309-338.
[66]	SUN J, DING Z, XIAO W, et al. Coupling between uplift of the Central Asian Orogenic Belt-NE Tibetan Plateau and accumulation of aeolian Red Clay in the inner Asia began at -7 Ma[J]. Earth-Science Reviews, 2022, 226: 103919. DOI URL
[67]	黄建平, 刘晓岳, 何永胜, 等. 氧循环与宜居地球[J]. 中国科学(地球科学), 2021, 51(4): 487-506.
[68]	李新, 刘丰, 方苗. 模型与观测的和弦:地球系统科学中的数据同化[J]. 中国科学(地球科学), 2020, 50(9): 1185-1194.
[69]	段蕾, 康沛竹. 走向社会主义生态文明新时代——论习近平生态文明思想的背景、内涵与意义[J]. 科学社会主义, 2016(2): 127-132.
[70]	张洪玮. 习近平生态文明思想的理论体系和时代价值研究[D]. 长春: 吉林大学, 2022.
[71]	马俊杰, 程捷. 自然文化概论[M]. 北京: 地质出版社, 2022.
[72]	杜文学. 青海省化隆县夏琼寺景区地质灾害发育特征及成因机制研究[J]. 西北师范大学学报(自然科学版), 2020, 56(1): 129-134.
[73]	王宝军, 陈骏, 胡文瑄. 基于地球系统科学理念的新型地质学人才培养改革[J]. 中国大学教学, 2022(8): 27-30.
[74]	汪品先. 对地球系统科学的理解与误解——献给第三届地球系统科学大会[J]. 地球科学进展, 2014, 29(11): 1277-1279. DOI
[75]	罗照华. 流体地球科学与地球系统科学[J]. 地学前缘, 2018, 25(6): 277-282. DOI
[76]	郭锋涛, 段玉山, 周维国, 等. 研学旅行课程标准(二)——课程结构、课程内容[J]. 地理教学, 2019(6): 4-7.