Indication capability for karst development elevation by knickpoints in Daba Mountain (Southwest China)

IF 1.1 4区 地球科学 Q3 GEOLOGY Carbonates and Evaporites Pub Date : 2024-02-23 DOI:10.1007/s13146-024-00922-z
Jiasen Zhang, Qiang Zhang, Ke Li, Zixuan Qin, Yanna Yang, Mo Xu
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Abstract

Regional tectonic uplift information is recorded by knickpoints distributed in multiple rivers. The changing base level (mainstream) caused by tectonic uplift also controls karst development. Groundwater should drain as springs near the base level due to karstification usually occurring near the base level, but some drains were higher than the present river in the canyon. The assumption is proposed that the spring is more elevated than the current river formed at the older intermittent stage in uplift processes and that knickpoints at the elevation can correspond to the springs. A typical basin south of Daba Mountain is selected to identify the assumption. Three knickpoints with 11 karst landforms suggest that knickpoints can indicate the karst development elevation in the basin. This method is promoted to 29 basins around Daba Mountain which are separated into DTB (North Daba Mountain Pre-Land Thrust Fault Belt) representing north part and DFB (South Daba Mountain Pre-Land Fold Belt) representing south part to verify the effectiveness of the assumption. The result discovers that the knickpoints and karst landforms have a similar high-frequency elevation interval in DFB and little variance in DTB. The reason may be that DFB has better karstification conditions, including precipitation and carbonate rock cover area, than DTB. Knickpoints is an effective indicator for karst development in area that has sufficient karstification condition like DFB. This study may provide a new perspective on the relationship between karst development and tectonic uplift and a method to find the karst groundwater drain elevation.

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大巴山(中国西南部)岩溶发育高程的节理点指示能力
分布在多条河流中的节理点记录了区域构造隆升的信息。构造隆升引起的基底面(主流)变化也控制着岩溶的发育。由于岩溶化通常发生在基底附近,地下水应在基底附近以泉水的形式排出,但有些排水沟比峡谷中现在的河流还要高。提出的假设是,在隆升过程中形成的较早的间歇阶段,泉水的海拔高度高于现在的河流,海拔高度上的节理点可以与泉水相对应。我们选择了大巴山以南的一个典型盆地来验证这一假设。三个节理点与 11 个岩溶地貌表明,节理点可以指示盆地的岩溶发育高程。该方法被推广到大巴山周围的 29 个盆地,这些盆地被分为代表北部的 DTB(北大巴山前陆相挤压断裂带)和代表南部的 DFB(南大巴山前陆相褶皱带),以验证该假设的有效性。结果发现,在 DFB 中,节理地貌和岩溶地貌的高频高程间隔相似,而在 DTB 中差异很小。其原因可能是 DFB 的降水量和碳酸盐岩覆盖面积等岩溶条件优于 DTB。在像 DFB 这样岩溶条件充分的地区,节理点是岩溶发育的有效指标。这项研究可为岩溶发育与构造隆升之间的关系提供一个新的视角,并为寻找岩溶地下水排泄高程提供一种方法。
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来源期刊
Carbonates and Evaporites
Carbonates and Evaporites 地学-地质学
CiteScore
2.80
自引率
14.30%
发文量
70
审稿时长
3 months
期刊介绍: Established in 1979, the international journal Carbonates and Evaporites provides a forum for the exchange of concepts, research and applications on all aspects of carbonate and evaporite geology. This includes the origin and stratigraphy of carbonate and evaporite rocks and issues unique to these rock types: weathering phenomena, notably karst; engineering and environmental issues; mining and minerals extraction; and caves and permeability. The journal publishes current information in the form of original peer-reviewed articles, invited papers, and reports from meetings, editorials, and book and software reviews. The target audience includes professional geologists, hydrogeologists, engineers, geochemists, and other researchers, libraries, and educational centers.
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