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高校地质学报 ›› 2025, Vol. 31 ›› Issue (04): 451-459.DOI: 10.16108/j.issn1006-7493.2024062

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广东黑排角岩滩蜂窝状洞穴形态特征及成因分析

胡良炜1,邓 飞1, 2*,罗锡宜1,潘时妹3   

  1. 1. 广东省佛山地质局,佛山 528000;
    2. 同济大学土木工程学院,上海 200092;
    3. 广西壮族自治区地质调查院,南宁 530023
  • 出版日期:2025-08-20 发布日期:2025-08-20

Morphological Characteristics and Genesis Analysis of Honeycombs on Heipaijiao Rocky Beach in Huidong County of Guangdong Province

HU Liangwei1,DENG Fei1, 2*,LUO Xiyi1,PAN Shimei3   

  1. 1. Foshan Geological Bureau of Guangdong Province, Foshan 528000, China;'
    2. College of Civil Engineering, Tongji University, Shanghai 200092, China;
    3. Guangxi Geological Survey, Nanning 530023, China
  • Online:2025-08-20 Published:2025-08-20

摘要: 蜂窝状洞穴广泛分布于不同地区的岩石露头和石质建筑之上,形态独特,其研究对深刻认识岩石风化机制具有重要意
义,多年来是地貌学研究的热点问题。因为其空间发育广泛,形态和基岩性质各异,导致前人研究提出不同成因解释,争议较大。此前认识多来自对砂岩和砾岩地区的研究,但对于受构造作用影响强烈的变质岩上蜂窝状洞穴的研究尚较少报道。广东省惠东县黑排角岩滩的劈理化流纹岩上发育大量直径为数厘米的椭圆状蜂窝状洞穴,文章利用三维扫描仪对典型区域782个洞穴的形态特征进行扫描,建立三维模型,高精度还原其形貌,定量化洞穴形态和分布规律,讨论其控制因素与形成过程。结果表明:蜂窝状洞穴洞口直径多在10~15 cm以下;洞深多在3 cm以下。洞口扁率较大(0.15~0.6之间为主),形状以椭圆、极椭圆为主,受节理裂隙、面理发育所控制。蜂窝状洞穴发育早期的主导因素为盐风化作用,镜下可见岩石内部的孔洞雏形。当洞穴扩张导致表层矿物或岩石碎片脱落后形成凹坑,此时洞穴逐渐受到海水的冲刷与磨蚀,盐风化与海蚀作用共同促进洞穴的发育。后期洞穴间的薄壁被打破,洞穴间彼此逐渐贯通。形成一定规模后,内部会作为一个新的平面进行下一个发育周期。

关键词: 蜂窝状洞穴, 海岸, 盐风化, 劈理化流纹岩, 三维扫描模型

Abstract: Honeycombs with unique shapes are widely distributed on rock outcrops and stone buildings in different regions. The study of honeycombs is of great significance to the deep understanding of rock weathering mechanism, which has been a hot issue in Geomorphology Research for many years. Honeycombs have wide spatial development, different morphologies and bedrock properties, leading to previous studies proposing different genetic explanations, which are controversial. Previous studies mostly focused on sandstone and conglomerate area, but there are few reports on the study of honeycombs on metamorphic rocks strongly affected by tectonic activity. A large number of elliptical honeycombs with diameters of several centimeters are developed on the fractured rhyolite of Heipaijiao Rocky Beach, Huidong County, Guangdong Province. In this paper, three-dimensional scanner is used to scan the morphological characteristics of 782 caves in typical areas, to establish three-dimensional models, restore their morphology with high precision, quantify the morphology and distribution of caves, and discuss their control factors and formation processes. The results show that the diameter of honeycombs hole is mostly below 10-15 cm; The depth is mostly below 3 cm. The oblateness of the portal is relatively large (mainly between 0.15 and 0.6), and its shape is mainly elliptical and extremely elliptical, controlled by the development of joint fissures and foliation. The dominant factor in the early development of honeycombs is salt weathering. Under the microscope, the rudiments of holes in the rock can be seen. When the expansion of the cave causes the surface minerals or rock fragments to fall off and form pits, the cave is gradually eroded and eroded by seawater, and salt weathering and sea erosion ntly promote the development of the cave. In the later stage, the thin wall between caves was broken, and the caves gradually penetrated each other. After a certain scale is formed, the interior will be used as a new plane for the next development cycle. 

Key words: honeycombs, coast, salt weathering, cleavage rhyolite, three-dimensional scanning model

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