Journal of Structural Geology最新文献

{"title":"Structural control on the Southern Andean Nevados de Chillán geothermal system","authors":"Valentina Mura ,&nbsp;Gloria Arancibia ,&nbsp;John Browning ,&nbsp;David Healy ,&nbsp;Camila López-Contreras ,&nbsp;Diego Morata ,&nbsp;Santiago Maza ,&nbsp;Carlos Cardona","doi":"10.1016/j.jsg.2025.105380","DOIUrl":"10.1016/j.jsg.2025.105380","url":null,"abstract":"<div><div>Detailed structural analysis from representative outcrops is necessary to characterize geothermal reservoir dynamics. Here, we estimate fracture density and intensity, as well as the dimensional properties of individual fault and fracture sets in basement rocks of the Nevados de Chillán Geothermal System. We identified several important structural features that could be responsible for controlling local fluid flow; the high-angle sinistral Las Trancas Fault as well as a series of low-angle reverse faults within the Las Termas-Olla de Mote Fault system. Most fractures identified strike either NE-SW, NNE-SSW, and NNW-SSE. Analysis of fault-slip data, supported by seismicity, indicates the presence of a main transtensional regime with subhorizontal NE-trending σ₁. Structures sub-parallel to the present-day local maximum horizontal stress show significant dilation tendencies, whilst NW-SE fractures are less prone to dilation. NE and E-W high angle faults could be primary conduits facilitating the upward migration of hot fluids from reservoirs within crystalline and fractured rocks. The fracture length distribution was analysed using power law, negative exponential, and log-normal distribution. The power law with a scaling exponent of about −3 provides the best fit to the data. This study advances our understanding of the structural control of the geothermal reservoir and its associated fracture-controlled fluid circulation and thereby improves the prospectivity in the region by quantifying the optimum fracture sets for fluid flow.</div></div>","PeriodicalId":50035,"journal":{"name":"Journal of Structural Geology","volume":"196 ","pages":"Article 105380"},"PeriodicalIF":2.6,"publicationDate":"2025-02-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143654528","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Calcite twin stress and strain indicators for various polymineralic rocks and mortars","authors":"Arito Sakaguchi ,&nbsp;Kohei Ando","doi":"10.1016/j.jsg.2025.105369","DOIUrl":"10.1016/j.jsg.2025.105369","url":null,"abstract":"<div><div>This paper proposes new formula to estimate strain and stress of various polymineralic materials in low-temperature elastic condition. Sakaguchi et al. (2011) proposed that the average twin lamellae density (Dtw) (number of twins/mm) depends on the load affecting the entire sample, based on discrete element method simulations and triaxial compression tests in the elastic deformation range. However, their derived relational formula between stress and Dtw, based solely on hard sandstone from the Shimanto accretionary complex in SW Japan, is only applicable to rocks with similar Young's modulus. This study attempted to perform uniaxial compression tests on mortar samples mixed with synthetic calcite grains. The specimens with different Young's modulus from approximately 5.9 to 10 GPa can be made by varying the water/cement ratio using the high strength cement. Calcite synthesized in an autoclave does not contain primary twin lamellae. From the result of the uniaxial compression test, the Dtw increased from 0 to 212/mm. The Dtw depends on the load affecting the entire sample. The rate of increase of Dtw with load varies for specimens with different Young's modulus, but Dtw increases in direct proportion to strain for all specimens regardless of Young's modulus, as represented by:</div><div><span><span><span><math><mrow><mi>ε</mi><mo>=</mo><mn>0.0094</mn><mspace></mspace><mtext>Dtw</mtext><mspace></mspace><mo>–</mo><mspace></mspace><mn>0.20</mn><mspace></mspace><mrow><mo>(</mo><mrow><mo>±</mo><mspace></mspace><mn>0.105</mn></mrow><mo>)</mo></mrow><mtext>,</mtext></mrow></math></span></span></span>where, ε represents shortening strain (%). For a hard specimen without plastic deformation and with a known Young's modulus, the paleo-stress experienced by the specimen can be estimated from the strain obtained from the average Dtw, since elastic strain and stress are proportional. This technique can be used for problems ranging from structural geology to building construction ones at low temperature and elastic strain state.</div></div>","PeriodicalId":50035,"journal":{"name":"Journal of Structural Geology","volume":"194 ","pages":"Article 105369"},"PeriodicalIF":2.6,"publicationDate":"2025-02-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143509153","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Differential salt-related structural deformation in the Eastern segment of the Qiulitage fold and thrust belt, Kuqa Foreland Basin: Evidences from seismic interpretation and numerical simulation analysis","authors":"Yingzhong Zhu ,&nbsp;Chuanxin Li ,&nbsp;Xinyi Jiang ,&nbsp;Yibo Zhao ,&nbsp;Gulifeire Tulujun ,&nbsp;Bencai Zhang","doi":"10.1016/j.jsg.2025.105372","DOIUrl":"10.1016/j.jsg.2025.105372","url":null,"abstract":"<div><div>The dymatic mechanisms of salt-related structural deformation in the foreland fold-and-thrust belts have been paid more and more attention for significance in hydrocarbon exploration. The Qiulitage Fold-and-Thrust Belt (QFTB) in the frontal Kuqa Foreland Basin(KFB) has been regarded as an important study area for its complicated deformation features and potential oil and gas resources. In the eastern QFTB, sub-salt fault-bend folds show a clear transition from a single row of basement-involved thrust belts in the east to a multi-row caprock detachment thrust belt in the west.This study uses discrete element numerical simulations, based on a geological model derived from seismic data, to validate and improve the model's reliability. This research investigates the factors controlling differential structural deformation in the QFTB. These simulations are mainly explored the impact of Jurassic-Triassic detachment layer thickness, stratal dip angle, and the role of dual salt layers. The results indicate that the detachment layer enhances the décollement thrusting effect, with thicker detachment layers leading to stronger décollement thrusting. If the detachment layer is too thin to support décollement thrusting, basement-involved faults develop instead. When the lower detachment layer is less than 800 m thick, two sets of basement-involved faults form, resulting in shorter thrust distances. Conversely, when this layer exceeds 800 m, only one set of basement-involved faults forms, along with two sets of caprock detachment faults at the frontal thrust belt, resulting in relatively greater thrust distances. Stratal dip angle is equivalent to the ancient topography which can restrain the formation and development of the thrust system, with steeper detachment layer angles reducing thrust distance and causing salt accumulation. In a dual-salt layer environment, the compaction of the overlying strata is weakened, which in turn enhances the décollement thrusting effect. The double salt layers of the Jidike and Kumugelemu Formations promote the development of multiple thrust fault arrays and enlarge the scale of frontal secondary anticlines. Therefore, the segmented differential deformation in the QFTB is influenced by the interplay of deep geological structures, detachment layers, and salt layer development. This study integrates seismic interpretation and numerical simulation to investigate the genetic mechanisms of segmented deformation in the QFTB, providing valuable insights and solid evidence for structural interpretation and hydrocarbon exploration in analogous salt-detachment systems.</div></div>","PeriodicalId":50035,"journal":{"name":"Journal of Structural Geology","volume":"194 ","pages":"Article 105372"},"PeriodicalIF":2.6,"publicationDate":"2025-02-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143509154","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Rapid crack-seal growth of Faden quartz","authors":"Estibalitz Ukar ,&nbsp;András Fall ,&nbsp;Stephen E. Laubach ,&nbsp;Richard Ketcham","doi":"10.1016/j.jsg.2025.105343","DOIUrl":"10.1016/j.jsg.2025.105343","url":null,"abstract":"<div><div>Faden quartz is characterized by a central thread-like fluid-inclusion-rich zone surrounded by a wide, clear, faceted rim. Typically found in fractures (veins) within low-temperature metamorphic rocks, the origins of Faden quartz remain contentious. We use scanning electron microscope-based cathodoluminescence and charge contrast imaging microscopy to reveal that Faden quartz threads consist of closely spaced, narrow microfractures (gap deposits) filled with quartz, which traps fluid inclusions and is surrounded by postkinematic lateral quartz deposits. Gap deposits form by the crack-seal mechanism of sequential breakage, fracture opening, and quartz precipitation. Faden quartz forms by the same mechanism as crack-seal quartz bridges found in some fractures formed under diagenetic conditions. Most fluid inclusions trapped within crack-seal gap deposits of Faden crystals from the Zhob region, Pakistan show a narrow range of homogenization temperatures between 140 °C and 147 °C and salinities of 3.5–5.0 wt% NaCl equivalents. Spanning quartz results in fracture-normal lengths of several tens of centimeters composed of narrow (5–10 μm) crack-seal deposits. Rapid widening relative to quartz accumulation and apertures enabled these fractures to remain open and function as fluid conduits in the subsurface for millions of years.</div></div>","PeriodicalId":50035,"journal":{"name":"Journal of Structural Geology","volume":"194 ","pages":"Article 105343"},"PeriodicalIF":2.6,"publicationDate":"2025-02-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143529321","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Spatial distribution of permeability in carbonate fault damage zones","authors":"Lukas Bernier ,&nbsp;Roger Soliva ,&nbsp;Delphine Roubinet ,&nbsp;Stéphane Dominguez ,&nbsp;Sylvain Mayolle ,&nbsp;Manon Bulliard ,&nbsp;Christopher Wibberley ,&nbsp;Tvrtko Korbar","doi":"10.1016/j.jsg.2025.105371","DOIUrl":"10.1016/j.jsg.2025.105371","url":null,"abstract":"<div><div>Fault conduits often localized fluid flow at specific sites related to fault segment growth and linkage. Understanding these mechanisms is essential for assessing geofluid pathways within reservoirs or leaks to the biosphere. We study here a segmented fault zone with strike-slip kinematics and pluri-decametric displacement, affecting carbonate rocks (Pag island, Croatia). This fault zone has multiple core zones surrounded by a damage zone (DZ), composed of different structures, including wall and link damage. To build discrete fracture networks (DFNs) of these structures, we conducted high-resolution fracture mapping and measurement of aperture in five areas around the main fault system. We also analyzed rock samples from each damage structure using the same method. Fluid flow simulations were performed through the DFNs to quantify the permeability and its anisotropy. We show that link damage is about 10² more permeable than the background damage, and 2 to 5 times more permeable than the wall damage. DZ permeability can be approximated by a tensor at the decametric-scale, but not at the centimetric-scale due to the strong permeability heterogeneity inherent to this scale. In the DZ, decametric-scale fracture patterns are 10–65 times more permeable than the centimetric-scale fractures, providing conduits for fluid flow. Finally, the maximum permeability strongly correlates with the product of mean aperture and connectivity, suggesting that these parameters could be used as proxy of the permeability in fault DZ. These results allow better estimation of fault zone permeability, providing constraints for flow modelling in various applications in the energy transition.</div></div>","PeriodicalId":50035,"journal":{"name":"Journal of Structural Geology","volume":"194 ","pages":"Article 105371"},"PeriodicalIF":2.6,"publicationDate":"2025-02-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143464454","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Investigating the Messinian salt in the Lebanese Levant basin: Insights into the geology and tectonics of the eastern Mediterranean region","authors":"Karam Sarieddine,&nbsp;Tony S. Nemer,&nbsp;Reenal Faysal","doi":"10.1016/j.jsg.2025.105368","DOIUrl":"10.1016/j.jsg.2025.105368","url":null,"abstract":"<div><div>The Messinian salt layer in the eastern Mediterranean region plays a key role in the Pliocene-Quaternary deformation and formation of the tectonic structures in the Levant Basin. The objective of this paper is to leverage 3D seismic reflection data from the northern Levant Basin offshore Lebanon in order to map the Messinian salt layer and understand its effect on the structures around it. For that, we used current 3D time seismic reflection data to investigate the seafloor and interpret the top and base of the salt layer, and we generated their corresponding bathymetric and structural maps. In addition, we generated isochron maps of the salt layer and the post-salt sedimentary section in an attempt to detect the variations in the lateral thicknesses of these layers. The presented maps helped to understand the impact of the Messinian salt deformation on the surrounding geological structures. We assess the distribution and geometries of the salt structures, and discuss the change in salt thickness across the basin. We also relate the halokinetic movement of the Messinian salt to the formation of bathymetric features along the seafloor. The results provide additional knowledge about the salt tectonics of the Messinian salt layer in the Levant Basin, and offer investigators to pursue further studies on the hydrocarbon potential in relation to the Messinian salt deformation.</div></div>","PeriodicalId":50035,"journal":{"name":"Journal of Structural Geology","volume":"194 ","pages":"Article 105368"},"PeriodicalIF":2.6,"publicationDate":"2025-02-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143438001","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Lateral growth, linkage and driving force of anticlines in the western Qaidam Basin, Northern Tibetan Plateau","authors":"Xiangdong Yang ,&nbsp;Lei Wu ,&nbsp;Bo Wang ,&nbsp;Jianchao Tang ,&nbsp;Wei Tan ,&nbsp;Xuhang Li ,&nbsp;Huitong Yang ,&nbsp;Kai Huang ,&nbsp;Junyong Zhang ,&nbsp;Xiubin Lin ,&nbsp;Ancheng Xiao ,&nbsp;Hanlin Chen","doi":"10.1016/j.jsg.2025.105370","DOIUrl":"10.1016/j.jsg.2025.105370","url":null,"abstract":"<div><div>In fold-and-thrust belts, folds usually grow laterally, and connect with neighboring folds to form larger structures. Whilst these processes significantly impact both the surface morphology and subsurface structures, there remains a gap in understanding the deep deformation involved in lateral growth and linkage of folds. To address this issue, our study focused on the northwestern Qaidam Basin hosting a series of well-exposed NW-SE-trending Cenozoic anticlines. We conducted a comprehensive analysis of the lateral growth and linkage patterns along with their subsurface structures of the anticlines, based on high-resolution remote-sensing images and seismic reflection data. Our investigation reveals that the anticlines are primarily décollement folds, with minor influence from basement-involved reverse faults. They have grown through lateral lengthening from their nuclei, with a generally faster propagation rate toward the southeast. This growth pattern is likely driven by the southeastward decrease in strain rate, coupled with the influence from southeastward tilting of the basement and topography in the Qaidam Basin. We identify six types of lateral linkage among anticlines in the Qaidam Basin: linear linkage, linear repulsion, oblique linkage, overlapped linkage, oblique non-linkage, and triple linkage. Notably, our study reports, for the first time, instances of linear repulsion and overlapped linkage, characterized by abnormally large distance to wavelength ratios. The development of linear repulsion is associated with the buried basement-involved fault between linked anticlines, whereas that of overlapped linkage likely results from rapid lateral growth of anticlines due to intense wind erosion. Moreover, our findings indicate that the en echelon-like distribution and arcuate shapes of the anticlines in the Qaidam Basin primarily stem from the lateral growth and linkage of the short-axis anticlines, rather than inferred basement strike-slip shears. The underlying driving force is the compression from the Qiman Tagh-East Kunlun Shan and the South Qilian Shan to the south and north, respectively. Our study underscores the interplay of décollements, basement-involved faults and erosional processes in shaping the diverse growth and linkage patterns of anticlines in fold-and-thrust belts.</div></div>","PeriodicalId":50035,"journal":{"name":"Journal of Structural Geology","volume":"193 ","pages":"Article 105370"},"PeriodicalIF":2.6,"publicationDate":"2025-02-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143420854","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Hydrogeological implications of fault-related folding in a Triassic braided sandstone","authors":"Timothy C. McMillan ,&nbsp;Titus Murray ,&nbsp;Martin S. Andersen ,&nbsp;Wendy A. Timms ,&nbsp;Gabriel C. Rau","doi":"10.1016/j.jsg.2025.105351","DOIUrl":"10.1016/j.jsg.2025.105351","url":null,"abstract":"<div><div>Although our understanding of how fault-related folds influence groundwater flow has advanced, the understanding of the exact geometries and architecture of displacement propagation is often uncertain. This paper focuses on fault-related folds (i.e., fault bend, fault propagation, and detachment folding) within a braided sandstone and their implications for groundwater flow due to the internal fracture architecture. To achieve this, we combine lineament mapping, field observations, 3D regional kinematic geological restoration modelling, and juxtaposition analysis of a major aquifer system in the Permo-Triassic Sydney Basin. Our lineament mapping allowed for targeted fieldwork where outcrop observations unveiled a mechanical stratigraphy (i.e. variations in mechanical properties, layer thickness, and frictional properties of mechanical boundaries) controlled by the braided river depositional architecture. This results in systematically spaced fracture sets and rotational shearing following the sedimentary fine-grained depositional variations causing brittle folding of the sandstone mass. Our 3D geological modelling quantitated the existence of regional fault-related fold geometries. We re-interpret these folded zones as broad fault damage zones, which are likely to promote vertical fracture flow through a rock matrix otherwise dominated by horizontal porous flow controlled by the depositional braided river environment. The conceptual model for potential for flow within the folded sandstone is then placed into the regional study context by fault juxtaposition analysis of displacements across the major regional aquifers separated by a regional aquitard assuming the geometry of a fault propagation fold. Such insights were notably absent from previous conceptual groundwater models for fault-related folds in braided river deposited sandstone successions. Our findings enhance the understanding of how mechanical stratigraphy can strongly influence the internal structures of fault-related folds and, in turn, affect the groundwater system connectivity.</div></div>","PeriodicalId":50035,"journal":{"name":"Journal of Structural Geology","volume":"193 ","pages":"Article 105351"},"PeriodicalIF":2.6,"publicationDate":"2025-02-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143420855","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Structural heterogeneities in fault-controlled cavity carbonate reservoirs: Insights into fracture and fault patterns","authors":"Duoming Zheng ,&nbsp;Lijuan Zhang ,&nbsp;Feng Shen","doi":"10.1016/j.jsg.2025.105358","DOIUrl":"10.1016/j.jsg.2025.105358","url":null,"abstract":"<div><div>This study investigates the role of fault zones and fracture networks in controlling cavity distribution and fluid flow within carbonate rocks of the Tarim Basin using static and dynamic data. By integrating multi-attribute unsupervised seismic facies analysis, fracture network modeling based on ant tracking, and slip and dilation tendency analyses, we construct 3D models to characterize fault zone patterns, cavity distribution, fracture geometry, connectivity, and deformation behavior. The results demonstrate that fault zone patterns are the primary controls on cavity distribution, with cavity arrangements closely reflecting the orientations and densities of fracture networks in the DFN model. Extensive cavity geobodies are concentrated at fault zone intersections, where fractures exhibit increased density and connectivity. The large geobody, defined by considerable connected volumes, high permeability, and high production performance, is situated in these intersections with dense, highly connected fracture networks. These networks enhance fluid flow and shape fluid pathways, highlighting their role in cavity reservoir dynamics. These findings provide insights for improving reservoir modeling and optimizing injection-related geoengineering activities, such as acid stimulation and hydraulic fracturing.</div></div>","PeriodicalId":50035,"journal":{"name":"Journal of Structural Geology","volume":"193 ","pages":"Article 105358"},"PeriodicalIF":2.6,"publicationDate":"2025-02-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143403133","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Late Quaternary left-slip rate of the Dangjiang segment along the Ganzi-Yushu-Xianshuihe Fault Zone in the central Tibetan Plateau and the tectonic implications","authors":"Zhongyuan Yu ,&nbsp;Baixu Chen ,&nbsp;Ping Song ,&nbsp;Qi Zhao ,&nbsp;Yicheng Wang ,&nbsp;Wenxuan Wang","doi":"10.1016/j.jsg.2025.105359","DOIUrl":"10.1016/j.jsg.2025.105359","url":null,"abstract":"<div><div>The Dangjiang segment, as the northwestern extremity of the NW-NNW-trending sinistral-slip Ganzi-Yushu-Xianshuihe Fault Zone (GYXFZ) in the central Tibetan Plateau, plays an important role in absorbing strain and regulating the relative movement between active blocks of the Tibetan Plateau interior. However, the late Quaternary strike-slip rate of the Dangjiang segment has rarely been studied because of extreme weather and hypoxia in high-altitude areas (H &gt; 5000 m) and inconvenient transportation, which directly affects the scientific understanding of the tectonic deformation style and reasonable assessment of the strong earthquake hazard along the GYXFZ and the analysis of the present deformation characteristics and geodynamic process of the plateau. Therefore, this study investigated the active tectonics of the Dangjiang segment based on integrated data from high-resolution satellite interpretation, large-scale geomorphic and geological mapping, trench excavations, and Quaternary chronological dating. The results reveal that the Dangjiang segment branches into the main Dangjiang Fault and secondary Zhiduo Fault, both of which have experienced intensive left-strike slip with minor dip movement since the late Quaternary. By measuring offset tributary terraces of the Tongtian River using a UAV survey, and dating their abandonment age using OSL and 14C with the upper terrace model, the late Quaternary strike-slip rate of the Dangjiang Fault and the Zhiduo Fault were estimated at ∼6.9 ± 0.1 mm/a and ∼2.1 ± 0.2 mm/a, respectively. Both the linear fitting value and the slip decomposition model indicate that the strike-slip rate of ∼8–10 mm/a in the late Quaternary is more consistent with geological and geomorphic estimations as well as geodetic constraints along the GYXFZ, and that the late Quaternary slip rate (∼8–10 mm/a) is consistent with the long-term and average slip rates along the structure. This spatiotemporal variation suggests that the current tectonic deformation of the Tibetan Plateau interior may have been continuous and distributed.</div></div>","PeriodicalId":50035,"journal":{"name":"Journal of Structural Geology","volume":"192 ","pages":"Article 105359"},"PeriodicalIF":2.6,"publicationDate":"2025-02-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143378442","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}