粤西北连州盆地构造演化对岩溶作用及岩溶塌陷的控制

樊燏; 黄琨; 段慧毓; 林宇航; 罗明明; 万军伟; 温汉辉; 曲金才; 张龙轩

doi:10.19509/j.cnki.dzkq.tb20230120

粤西北连州盆地构造演化对岩溶作用及岩溶塌陷的控制

doi: 10.19509/j.cnki.dzkq.tb20230120

1.
中国地质大学(武汉)环境学院, 武汉 430078
2.
广东省有色金属地质局九四○队, 广东清远 511500

基金项目:

国家自然科学基金项目 42172276

详细信息

作者简介:
樊燏, E-mail: yufan@cug.edu.cn

通讯作者:
万军伟, E-mail: wanjw@cug.edu.cn

中图分类号: P642.25
计量
- 文章访问数: 317
- PDF下载量: 58
- 被引次数: 0
出版历程
- 收稿日期: 2023-03-07
- 录用日期: 2023-09-01
- 修回日期: 2023-05-28

Control of tectonic evolution on karstification and karst collapse in the Lianzhou Basin, northwestern Guangdong Province

1.
School of Environmental Studies, China University of Geosciences(Wuhan), Wuhan 430078, China
2.
No. 940 Branch of Geology Bureau for Nonferrous Metals of Guangdong Province, Qingyuan Guangdong 511500, China

More Information

Author Bio:
FAN Yu, E-mail: yufan@cug.edu.cn

Corresponding author: WAN Junwei, E-mail: wanjw@cug.edu.cn

摘要

摘要:
目前对连州盆地中生代以来的形成演化及其与岩溶发育规律的响应关系尚缺乏系统性认识。基于最新地质调查、水文地质钻探、溶蚀试验和三维地质建模, 结合已有地质资料, 划分了盆地构造演化阶段并探讨了各阶段岩溶作用。前白垩纪, 在地壳升降运动下沉积较强溶蚀能力碳酸盐岩, 这为岩溶发育奠定了物质基础。印支运动促使垂向叠置地层形成EW向构造, 燕山运动导致其横跨-斜跨叠加NE-SW向构造, 这些地质构造控制碳酸盐岩地质结构和空间展布特征及溶蚀性能, 山脉和水系分布确立, 但岩溶整体不发育。白垩纪-古近纪发育陆内山间断陷汇流湖盆, 地壳缓慢隆升加强了盆地周围岩溶作用, 现保留早期岩溶台面。后期被冲洪积物埋藏-充填-固结成岩, 岩溶基本停止发育, 形成厚覆盖型红层盆地。新近纪以来, 地壳快速抬升导致盆地四周山体不断抬高, 河流深切, 岩溶强烈发育, 塑造多级岩溶台面。盆地内部分白垩系红层被剥蚀或切穿, 岩溶作用复活, 水系经多次变迁和贯通后, 形成第四系浅覆盖型岩溶断陷盆地。构造演化控制岩溶发育规律, 岩溶作用影响盆地内部结构, 土体结构孕育岩溶地面塌陷。研究成果可为认识覆盖型岩溶区岩溶塌陷条件提供科学依据和指导。
- 连州盆地 /
- 构造演化 /
- 地壳活动 /
- 岩溶作用 /
- 岩溶塌陷
Abstract: Objective
There is still a lack of systematic understanding of the evolution process of the Lianzhou Basin since the Mesozoic and its response to karstic development.
Methods
Based on the comprehensive analysis of the latest field geological investigations, hydrogeological drilling, dissolution experiments, and three-dimensional geological modelling, the tectonic evolution stages of the basin can be divided, and the karstification of each stage can be discussed by considering the existing geological data.
Results
Before the Cretaceous, carbonate rocks with strong dissolution were successively deposited under the rise or fall movement of the crust, which laid a material foundation for karstic development. The Indosinian movement caused vertically multilayered strata to form an E-W-trending structure, and the Yanshanian movement made the straddle-oblique superimposed a NE-SW-trending structure. They controlled the geological structures, spatial distribution, and dissolution behaviors of carbonate strata. And the distribution of mountains and river system were established. However, karst generally does not develop. An intracontinental and intermountain faulted confluence lake basin formed from the Cretaceous to the Palaeogene, the slow crustal uplift strengthened the karstification around the basin, and it currently retains the early karst platform. Later, they were buried-filled-consolidated by alluvial deposits; therefore, karst basically stopped developing, generating a thick-covered red strata basin. Since the Neogene, the rapid uplift of the crust has led to the continuous elevation of mountains around the basin, deepening of rivers, and strong development of karst, shaping multilevel karst platforms. When part of the Cretaceous red strata in the basin are denuded or cut through, karstification is reactivated. After many changes and penetrations of water systems, the graben basin formed, with karst strata covered by Quaternary sediments, Tectonic evolution controls karstic development, karstification influences the internal structure of the basin, and soil structure causes karst ground collapse.
Conclusion
This study can provide a scientific basis and guidance for understanding karst collapse conditions in covered karst areas.
- Lianzhou Basin /
- tectonic evolution /
- crustal movement /
- karstification /
- karst collapse
注释:

所有作者声明不存在利益冲突。

HTML全文

图 1 研究区岩溶水文地质概图

Figure 1. Karst hydrogeological map of the study area

下载: 全尺寸图片幻灯片

图 2 已发岩溶塌陷特征

Figure 2. Karst collapse characteristics

下载: 全尺寸图片幻灯片

图 3 连州盆地云灰岩、灰云岩与灰岩、白云岩溶蚀度R_si(a, c)和化学溶蚀度R_di(b, d)随时间变化曲线

Figure 3. Curves of the dissolution rate (a, c) and chemical dissolution rate (b, d) of dolomitic limestone, calcite dolomite, limestone and dolomite over time in the lianzhou Basin

下载: 全尺寸图片幻灯片

图 4 连州市主城区第四系覆盖层三维地质结构模型

Figure 4. Three-dimensional geological structure of Quaternary covered layers in main urban area of Lianzhou City

下载: 全尺寸图片幻灯片

图 5 连州市主城区垂向岩溶发育规律

Figure 5. Vertical karst development law in main urban area of Lianzhou City

下载: 全尺寸图片幻灯片

图 6 枯、丰水期岩溶地下水位等值线图

Figure 6. Contour map of karst groundwater level in dry(a) and wet(b) seasons

下载: 全尺寸图片幻灯片

图 7 连州盆地构造形成演化过程与岩溶作用示意图

T₁d².大冶组二段；T₁d¹.大冶组一段；P₂t.童子岩组; P₁q-m.栖霞-茅口组；C₂h.壶天组；C₁z.梓门桥组；C₁c.测水组；C₁s.石磴子组；C₁l.连县组；D₃r.融县组；下同

Figure 7. Schematic diagram of tectonic evolution formation and karstification in Lianzhou Basin

下载: 全尺寸图片幻灯片

图 8 发育的岩溶洞穴野外出露特征

Figure 8. Occurrences of karst caves developed in the wild

下载: 全尺寸图片幻灯片

图 9 受NNE向裂隙和近EW向断裂发育的溶洞野外特征

Figure 9. Exposed characteristics of karst caves developed by NNE-trending fissures or EW-trending faults

下载: 全尺寸图片幻灯片

图 10 岩溶塌陷灾害点形成条件特征

a.地下水主径流带黏性土软化塑性变形; b.碳酸盐岩与非碳酸盐岩交界带砂性土渗透变形; c.地下水排泄带砂性土渗透变形

Figure 10. Formation condition characteristics of karst collapse disaster points

下载: 全尺寸图片幻灯片

表 1 连州盆地碳酸盐岩溶蚀试验结果

Table 1. Corrosion test results of carbonatite rocks in the Lianzhou Basin

地层	岩性描述	矿物组成φ_B/%			比溶蚀度K_v		比化学溶蚀度K_cv
地层	岩性描述	方解石	白云石	酸不溶物	5次试验均值	地层均值	5次试验均值	地层均值
大冶组一段	灰色薄-中厚层状微晶泥质灰岩	79.18	3.84	16.98	0.79	0.79	0.92	0.92
栖霞组-茅口组	深灰色厚层状含燧石微晶灰岩	95.45	3.00	1.55	0.93	0.93	0.93	1.01
壶天组	灰色厚层微晶灰岩	97.51	1.01	1.48	1.00	1.03	0.85	0.98
壶天组	灰白色厚层微晶白云岩	2.22	95.63	2.15	1.06	1.03	1.11	0.98
梓门桥组	灰色厚层微晶灰质白云岩	28.13	69.78	2.09	0.75		0.78
	灰色厚层微晶灰质白云岩	43.92	54.58	1.50	1.13		0.98
	灰色厚层微晶含灰质白云岩	24.10	68.03	7.87	1.30		0.97
	灰色厚层微晶灰质白云岩	24.99	72.43	2.58	1.26	1.04	1.18	0.97
	深灰色中厚层细晶含灰质白云岩	7.67	90.50	1.83	1.06		1.06
	灰黑色厚层细晶灰质白云岩	25.48	71.28	3.24	0.92		0.89
	灰黑色厚层含炭质微晶灰岩	96.45	1.99	1.57	0.88		0.94
石磴子组	灰黑色薄-中层微晶灰岩	71.41	1.55	27.04	1.03		1.06
	灰黑色厚层含炭质细晶灰岩	94.58	2.05	3.37	0.84		0.90
	灰黑色厚层微晶含白云质灰岩	86.88	10.09	3.03	0.94	0.92	1.11	1.02
	深灰色厚层微晶白云岩	4.01	91.39	4.60	0.83		1.01
	灰黑色薄-中层微晶纯灰岩	93.72	3.36	2.92	0.95		1.00
连县组	灰黑色厚层细晶含白云质灰岩	83.01	14.81	2.18	0.99		0.93
	灰色厚层细晶含白云质灰岩	86.36	6.43	7.20	1.05		1.14
	灰黑色厚层细晶含白云质灰岩	80.57	17.79	1.64	1.05	0.99	1.17	1.07
	灰黑色厚层细晶白云岩	4.13	94.89	0.98	0.87		1.00
	浅灰色厚层微晶含灰质白云岩	10.67	86.08	3.25	0.99		1.13
融县组	深灰色厚层细晶白云质灰岩	63.46	32.39	4.15	1.48	1.22	1.04	1.03
	深灰色薄-中厚层细晶灰岩	87.97	7.97	6.78	1.00		0.97
	深灰色厚层微晶豹皮灰岩	89.33	3.89	6.78	1.08		1.04
	深灰色厚层微晶含白云质灰岩	81.89	9.78	8.33	1.32		1.05

下载: 导出CSV

参考文献(60)

[1]	廖镜彪, 王雪梅, 李玉欣, 等. 城市化对广州降水的影响分析[J]. 气象科学, 2011, 31(4): 384-390. doi: 10.3969/j.issn.1009-0827.2011.04.004 LIAO J B, WANG X M, LI Y X, et al. An analysis study of the impacts of urbanization on precipitation in Guangzhou[J]. Journal of the Meteorological Sciences, 2011, 31(4): 384-390. (in Chinese with English abstract) doi: 10.3969/j.issn.1009-0827.2011.04.004
[2]	陈秀洪, 刘丙军, 李源, 等. 城市化建设对广州夏季降水过程的影响[J]. 水文, 2017, 37(1): 25-32. https://www.cnki.com.cn/Article/CJFDTOTAL-SWZZ201701005.htm CHEN X H, LIU B J, LI Y, et al. Impact of urbanization on summer precipitation process in Guangzhou[J]. Journal of China Hydrology, 2017, 37(1): 25-32. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-SWZZ201701005.htm
[3]	黄国如, 陈易偲, 姚芝军. 高度城镇化背景下珠三角地区极端降雨时空演变特征[J]. 水科学进展, 2021, 32(2): 161-170. https://www.cnki.com.cn/Article/CJFDTOTAL-SKXJ202102001.htm HUANG G R, CHEN Y S, YAO Z J. Spatial and temporal evolution characteristics of extreme rainfall in the Pearl River Delta under high urbanization[J]. Advances in Water Science, 2021, 32(2): 161-170. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-SKXJ202102001.htm
[4]	FARRANT A R, COOPER A H. Karst geohazards in the UK: The use of digital data for hazard management[J]. Quarterly Journal of Engineering Geology & Hydrogeology, 2008, 41(3): 339-356.
[5]	PAPADOPOULOU-VRYNIOTI K, BATHRELLOS G D, SKILODIMOU H D, et al. Karst collapse susceptibility mapping considering peak ground acceleration in a rapidly growing urban area[J]. Engineering Geology, 2013, 158: 77-88. doi: 10.1016/j.enggeo.2013.02.009
[6]	MAO Z Y, JIAO Y Y, TAN F, et al. Susceptibility mapping of ground collapse caused by anthropogenic activities[J/OL]. Journal of Earth Science, https://new.cnki.net/kcms/detail/42.1788.P.20220307.1002.003.html
[7]	WHITE W B. Karst hydrology: Recent developments and open questions[J]. Engineering Geology, 2002, 65(2/3): 85-105.
[8]	FORD D C, WILLIAMS P W. Karst hydrogeology and geomorphology[M]. Chichester: Wiley, 2007.
[9]	HARTMANN A, GOLDSCHEIDER N, WAGENER T, et al. Karst water resources in a changing world: Review of hydrological modeling approaches[J]. Reviews of Geophysics, 2014, 52(3): 218-242. doi: 10.1002/2013RG000443
[10]	袁道先, 蒋勇军, 沈立成, 等. 现代岩溶学[M]. 北京: 科学出版社, 2016. YUAN D X, JIANG Y J, SHEN L C, et al. Modern karstology[M]. Beijing: Science Press, 2016. (in Chinese)
[11]	徐亚东, 梁银平, 江尚松, 等. 中国东部新生代沉积盆地演化[J]. 地球科学, 2014, 39(8): 1079-1098. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201408011.htm XU Y D, LIANG Y P, JIANG S S, et al. Evolution of Cenozoic sedimentary basins in eastern China[J]. Earth Science, 2014, 39(8): 1079-1098. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201408011.htm
[12]	张宗言, 何卫红, 韦一, 等. 下扬子中生代沉积盆地演化[J]. 地球科学, 2014, 39(8): 1017-1034. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201408007.htm ZHANG Z Y, HE W H, WEI Y, et al. Evolution of Mesozoic sedimentary basins in the Lower Yangtze[J]. Earth Science, 2014, 39(8): 1017-1034. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201408007.htm
[13]	郑金云, 高阳东, 张向涛, 等. 珠江口盆地构造演化旋回及其新生代沉积环境变迁[J]. 地球科学, 2022, 47(7): 2374-2390. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX202207007.htm ZHENG J Y, GAO Y D, ZHANG X T, et al. Tectonic evolution cycles and Cenozoic sedimentary environment changes in Pearl River Mouth Basin[J]. Earth Science, 2022, 47(7): 2374-2390. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX202207007.htm
[14]	颜慧明, 常威, 郭绪磊, 等. 岩溶水流系统识别方法及其在引调水工程隧洞选线中的应用[J]. 地质科技通报, 2022, 41(1): 127-136. 10.19509/j.cnki.dzkq.2022.0008 YAN H M, CHANG W, GUO X L, et al. Identification of the karst water flow system and its application in the tunnel line selection of water diversion projects[J]. Bulletin of Geological Science and Technology, 2022, 41(1): 127-136. (in Chinese with English abstract) 10.19509/j.cnki.dzkq.2022.0008
[15]	颜慧明, 常威, 季怀松, 等. 黄陵背斜东北翼岩溶水系统特征及其对引调水隧洞工程的影响[J]. 地质科技通报, 2022, 41(5): 315-323. 10.19509/j.cnki.dzkq.2022.0165 YAN H M, CHANG W, JI H S, et al. Characteristics of the karst water system on the northeast wing of the Huangling anticline and its impact on water diversion tunnel engineering[J]. Bulletin of Geological Science and Technology, 2022, 41(5): 315-323. (in Chinese with English abstract) 10.19509/j.cnki.dzkq.2022.0165
[16]	马超, 曾斌, 罗明明, 等. 武汉两湖隧道岩溶水系统结构及水循环规律[J]. 地质科技通报, 2022, 41(5): 395-404. doi: 10.19509/j.cnki.dzkq.2022.0198 MA C, ZENG B, LUO M M, et al. Structure of karst water system and hydrological circulation characteristics of Lianghu Tunnel in Wuhan[J]. Bulletin of Geological Science and Technology, 2022, 41(5): 395-404. (in Chinese with English abstract) doi: 10.19509/j.cnki.dzkq.2022.0198
[17]	吴远斌, 刘之葵, 殷仁朝, 等. 湖南怀化盆地岩溶发育特征与分布规律[J]. 中国岩溶, 2022, 41(5): 759-772. https://www.cnki.com.cn/Article/CJFDTOTAL-ZGYR202205008.htm WU Y B, LIU Z K, YIN R C, et al. Karst development characteristics and distribution law in Huaihua Basin, Hunan Province[J]. Carsologica Sinica, 2022, 41(5): 759-772. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-ZGYR202205008.htm
[18]	尹欧, 何阳, 李彬, 等. 区域构造特征与岩溶发育空间分布关系研究: 以长沙市煤炭坝地区为例[J]. 地下水, 2021, 43(1): 114-116. https://www.cnki.com.cn/Article/CJFDTOTAL-DXSU202101040.htm YIN O, HE Y, LI B, et al. Study on the relationship between regional tectonic framework and spatial distribution of karst: Taking the coal dam area of Changsha as an example[J]. Ground Water, 2021, 43(1): 114-116. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DXSU202101040.htm
[19]	樊燏, 常威, 魏世毅, 等. 聚龙山向斜三叠系含水层岩溶发育史及地下水流场控制意义[J]. 地质科技通报, 2022, 41(5): 377-385. 10.19509/j.cnki.dzkq.2022.0160 FAN Y, CHANG W, WEI S Y, et al. History of karstification and groundwater flow field within Triassic water-bearing strata in Julongshan syncline[J]. Bulletin of Geological Science and Technology, 2022, 41(5): 377-385. (in Chinese with English abstract) 10.19509/j.cnki.dzkq.2022.0160
[20]	雷明堂, 蒋小珍. 岩溶塌陷研究现状、发展趋势及其支撑技术方法[J]. 中国地质灾害与防治学报, 1998, 9(3): 1-6. https://www.cnki.com.cn/Article/CJFDTOTAL-ZGDH199803000.htm LEI M T, JIANG X Z. Research on the present situation and developing tendency of karst collapse and techniques for its supporting[J]. The Chinese Journal of Geological Hazard and Control, 1998, 9(3): 1-6. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-ZGDH199803000.htm
[21]	BASSO A, BRUNO E, PARISE M, et al. Morphometric analysis of sinkholes in a karst coastal area of southern Apulia (Italy)[J]. Environmental Earth Sciences, 2013, 70(6): 2545-2559. doi: 10.1007/s12665-013-2297-z
[22]	KAUFMANN G, ROMANOV D. Structure and evolution of collapse sinkholes: Combined interpretation from physico-chemical modelling and geophysical field work[J]. Journal of Hydrology, 2016, 540: 688-698. doi: 10.1016/j.jhydrol.2016.06.050
[23]	罗小杰, 罗程. 岩溶地面塌陷三机理理论及其应用[J]. 中国岩溶, 2021, 40(2): 171-188. https://www.cnki.com.cn/Article/CJFDTOTAL-ZGYR202102001.htm LUO X J, LUO C. Three-Mechanism Theory (TMT) of karst ground collapse and its application[J]. Carsologica Sinica, 2021, 40(2): 171-188. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-ZGYR202102001.htm
[24]	SALEM H S. Multi-and inter-disciplinary approaches towards understanding the sinkholes'phenomenon in the Dead Sea Basin[J]. SN Applied Sciences, 2020, 2(4): 667.
[25]	NAM B H, KIM Y J, YOUN H. Identification and quantitative analysis of sinkhole contributing factors in Florida's Karst[J]. Engineering Geology, 2020, 271: 105610.
[26]	FRUMKIN A, EZERSKY M, AL-ZOUBI A, et al. The dead sea sinkhole hazard: Geophysical assessment of salt dissolution and collapse[J]. Geomorphology, 2011, 134(1/2): 102-117.
[27]	SAMYN K, MATHIEU F, BITRI A, et al. Integrated geophysical approach in assessing karst presence and sinkhole susceptibility along flood-protection dykes of the Loire River, Orléans, France[J]. Engineering Geology, 2014, 183: 170-184.
[28]	CARBONEL D, RODRÍGUEZ-TRIBALDOS V, GUTIÉ-RREZ F, et al. Investigating a damaging buried sinkhole cluster in an urban area (Zaragoza City, NE Spain) integrating multiple techniques: Geomorphological surveys, DInSAR, DEMs, GPR, ERT, and trenching[J]. Geomorphology, 2015, 229: 3-16.
[29]	WANG X M, WANG S M, PENG X Y, et al. Equivalent numerical simulation method and application in karst-induced collapse of overlying sandy stratum[J]. Engineering Failure Analysis, 2022, 137: 106280.
[30]	武鑫, 王艺霖, 黄敬军, 等. 徐州地区碳酸盐岩溶蚀特征及影响因素分析[J]. 地质科技情报, 2019, 38(3): 120-126. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201903011.htm WU X, WANG Y L, HUANG J J, et al. Dissolution characteristics of carbonate and analysis of the key influence factors in Xuzhou region[J]. Geological Science and Technology Information, 2019, 38(3): 120-126. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201903011.htm
[31]	中国科学院地质研究所岩溶研究组. 中国岩溶研究[M]. 北京: 科学出版社, 1979. Karst Research Group, Institute of Geology, Chinese Academy of Sciences. Karst Research in China[M]. Beijing: Science Press, 1979. (in Chinese)
[32]	何宇彬, 金玉璋, 李康. 碳酸盐岩溶蚀机理研究[J]. 中国岩溶, 1984, 3(2): 12-16. https://www.cnki.com.cn/Article/CJFDTOTAL-ZGYR198402001.htm HE Y B, JIN Y Z, LI K. An experimental study of carbonate rock corrosion mechanism[J]. Carsologica Sinica, 1984, 3(2): 12-16. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-ZGYR198402001.htm
[33]	韩庆之, 梁杏, 曾克峰, 等. 碳酸盐岩可溶性室内研究[J]. 地质科技情报, 1998, 17(增刊2): 102-106. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ8S2.018.htm HAN Q Z, LIANG X, ZENG K F, et al. Study on solubility of carbonate rock in door[J]. Geological Science and Technology Information, 1998, 17(S2): 102-106. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ8S2.018.htm
[34]	LUO M M, ZHOU H, LIANG Y P, et al. Horizontal and vertical zoning of carbonate dissolution in China[J]. Geomorphology, 2018, 322: 66-75.
[35]	陈如冰, 罗明明, 罗朝晖, 等. 三峡地区碳酸盐岩化学组分与溶蚀速率的响应关系[J]. 中国岩溶, 2019, 38(2): 258-264. https://www.cnki.com.cn/Article/CJFDTOTAL-ZGYR201902014.htm CHEN R B, LUO M M, LUO Z H, et al. Response relationship between chemical composition and dissolution rate of carbonate rocks in the Three Gorges Area[J]. Carsologica Sinica, 2019, 38(2): 258-264. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-ZGYR201902014.htm
[36]	南颐, 潘洪标, 水涛, 等. 广东1: 20万连县幅区域地质调查报告书[R]. 广州: 广东省地质局, 1973. NAN Y, PAN H B, SHUI T, et al. 1: 200000 regional geological survey report of Lianxian sheet in Guangdong Province[R]. Guangzhou: Guangdong Geological Bureau, 1973. (in Chinese)
[37]	广东省地质矿产局. 广东省区域地质志[M]. 北京: 地质出版社, 1988. Guangdong Bureau of Geology and Mineral Resources. Regional geology of Guangdong Province[M]. Beijing: Geological Publishing House, 1988. (in Chinese)
[38]	柏道远, 贾宝华, 钟响, 等. 湘东南印支运动变形特征研究[J]. 地质论评, 2012, 58(1): 19-29. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201201002.htm BAI D Y, JIA B H, ZHONG X, et al. Study on the deformation of Indosinian movement in southeastern Hunan[J]. Geological Review, 2012, 58(1): 19-29. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201201002.htm
[39]	褚杨, 林伟, FAURE M, 等. 华南板块早中生代陆内造山过程: 以雪峰山-九岭为例[J]. 岩石学报, 2015, 31(8): 2145-2155. https://cpfd.cnki.com.cn/Article/CPFDTOTAL-DZDQ201601003009.htm CHU Y, LIN W, FAURE M, et al. Early Mesozoic intracontinental orogeny: Example of the Xuefengshan-Jiuling belt[J]. Acta Petrologica Sinica, 2015, 31(8): 2145-2155. (in Chinese with English abstract) https://cpfd.cnki.com.cn/Article/CPFDTOTAL-DZDQ201601003009.htm
[40]	马永生, 陈洪德, 王国力, 等. 中国南方构造-层序岩相古地理图集[R]. 北京: 科学出版社, 2009. MA Y S, CHEN H D, WANG G L, et al. Tectonic-sequence lithofacies paleogeography atlas of southern China[R]. Beijing: Science Press, 2009. (in Chinese)
[41]	王清晨, 蔡立国. 中国南方显生宙大地构造演化简史[J]. 地质学报, 2007, 81(8): 1025-1040. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200708002.htm WANG Q C, CAI L G. Phanerozoic tectonic evolution of South China[J]. Acta Geologica Sinica, 2007, 81(8): 1025-1040. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200708002.htm
[42]	LI J H, ZHANG Y Q, DONG S W, et al. Late Mesozoic-Early Cenozoic deformation history of the Yuanma Basin, central South China[J]. Tectonophysics, 2012, 570/571: 163-183.
[43]	高中亮, 王艳飞, 雷胜兰, 等. 珠江口盆地CO₂分布特征与成藏机制浅析[J]. 地质科技通报, 2022, 41(4): 57-68. doi: 10.19509/j.cnki.dzkq.2022.0204 GAO Z L, WANG Y F, LEI S L, et al. Distribution characteristics and accumulation mechanism of carbon dioxide gas reservoirs in the Pearl River Mouth Basin[J]. Bulletin of Geological Science and Technology, 2022, 41(4): 57-68. (in Chinese with English abstract) doi: 10.19509/j.cnki.dzkq.2022.0204
[44]	陈佩蓉, 许中杰, 孔锦涛, 等. 闽西南地区中侏罗世古气候演化及其对华南构造体制转换的响应[J]. 大地构造与成矿学, 2020, 44(5): 1012-1024. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK202005015.htm CHEN P R, XU Z J, KONG J T, et al. Paleoclimatic evolution during Middle Jurassic in southwestern Fujian and its responses to the tectonic regime transition in South China[J]. Geotectonica et Metallogenia, 2020, 44(5): 1012-1024. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK202005015.htm
[45]	HU R L, YEUNG M R, LEE C F, et al. Regional risk assessment of karst collapse in Tangshan, China[J]. Environmental Geology, 2001, 40(11/12): 1377-1389.
[46]	董树文, 张岳桥, 龙长兴, 等. 中国侏罗纪构造变革与燕山运动新诠释[J]. 地质学报, 2007, 81(11): 1449-1461. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200711002.htm DONG S H, ZHANG Y Q, LONG C X, et al. Jurassic tectonic revolution in China and new interpretation of the Yanshan Movement[J]. Acta Geologica Sinica, 2007, 81(11): 1449-1461. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200711002.htm
[47]	SETON M, MÜLLER R D, ZAHIROVIC S, et al. Global continental and ocean basin reconstructions since 200 Ma[J]. Earth-Science Reviews, 2012, 113(3/4): 212-270.
[48]	DONG Y P, SANTOSH M. Tectonic architecture and multiple orogeny of the Qinling Orogenic Belt, Central China[J]. Gondwana Research, 2016, 29(1): 1-40.
[49]	DONG Y P, YANG Z, LIU X M, et al. Mesozoic intracontinental orogeny in the Qinling Mountains, central China[J]. Gondwana Research, 2016, 30: 144-158.
[50]	贾磊. 粤西北连州地区印支-燕山运动变形特征研究[J]. 西部资源, 2017, 3: 23-25. https://www.cnki.com.cn/Article/CJFDTOTAL-XBZY201703011.htm JIA L. Study on the deformation of Indosinian to Yanshanian Movement in Lianzhou, Northwest Guangdong[J]. Western Resources, 2017, 3: 23-25. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-XBZY201703011.htm
[51]	HU G, HU W X, CAO J, et al. Deciphering the Early Cretaceous transgression in coastal southeastern China: Constraints based on petrography, paleontology and geochemistry[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2012, 317/318: 182-195.
[52]	LI J H, CAWOOD P A, RATSCHBACHER L, et al. Building Southeast China in the Late Mesozoic: Insights from alternating episodes of shortening and extension along the Lianhuashan fault zone[J]. Earth-Science Reviews, 2020, 201: 103056.
[53]	ZHOU X M, LI W X. Origin of Late Mesozoic igneous rocks in southeastern China: Implications for lithosphere subduction and underplating of mafic magmas[J]. Tectonophysics, 2000, 326(3/4): 269-287.
[54]	何岸北. 东南沿海古海岸山脉演化: 永安盆地晚中生代沉积及古气候响应[D]. 广州: 中国科学院广州地球化学研究所, 2022: 53-88. HE A B. Evolution of paleo-coastal mountains along the southeast coast: Sedimentation and paleoclimate response in Yong'an Basin of the Late Mesozoic[D]. Guangzhou: Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, 2022: 53-88. (in Chinese with English abstract)
[55]	王文艳, 刘秀铭, 马明明, 等. 南雄盆地白垩纪红层沉积环境分析[J]. 亚热带资源与环境学报, 2016, 11(3): 29-37. https://www.cnki.com.cn/Article/CJFDTOTAL-FJDL201603005.htm WANG W Y, LIU X M, MA M M, et al. Sedimentary environment of Cretaceous red beds in Nanxiong Basin, Guangdong Province[J]. Journal of Subtropical Resources and Environment, 2016, 11(3): 29-37. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-FJDL201603005.htm
[56]	许志琴, 王勤, 李忠海, 等. 印度-亚洲碰撞: 从挤压到走滑的构造转换[J]. 地质学报, 2016, 90(1): 1-23. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201601001.htm XU Z Q, WANG Q, LI Z H, et al. Indo-Asian collision: Tectonic transition from compression to strike slip[J]. Acta Geologica Sinica, 2016, 90(1): 1-23. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201601001.htm
[57]	谢树鑫, 罗建鸿, 黄录太, 等. 广东1: 20万连县幅区域水文地质普查报告书[R]. 广州: 广东省地质局, 1981. XIE S X, LUO J H, HUANG L T, et al. 1: 200000 regional hydrogeologic survey report of Lianxian sheet in Guangdong Province[R]. Guangzhou: Guangdong Geological Bureau, 1981. (in Chinese)
[58]	WANG Y, WANG Y J, LI S B, et al. Exhumation and landscape evolution in eastern South China since the Cretaceous: New insights from fission-track thermochronology[J]. Journal of Asian Earth Sciences, 2020, 191: 104239.
[59]	CLIFT P D, BLUSZTAJN J, NGUYEN A D. Large-scale drainage capture and surface uplift in eastern Tibet-SW China before 24 Ma inferred from sediments of the Hanoi Basin, Vietnam[J]. Geophysical Research Letters, 2006, 33(19): L19403.
[60]	闫义, ALI A A A, 田陟贤, 等. 南海北缘盆-岭格局及地貌演化过程[J]. 热带海洋学报, 2016, 35(6): 46-57. https://www.cnki.com.cn/Article/CJFDTOTAL-RDHY201606006.htm YAN Y, ALI A A A, TIAN Z X, et al. Basin-mountain evolution, thermo-tectonic history and surface crustal recycling processes of the northern margin of the South China Sea[J]. Journal of Tropical Oceanography, 2016, 35(6): 46-57. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-RDHY201606006.htm