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Active tectonics in the Himalayan foreland due to an advancing detachment plane 喜马拉雅前陆的活动构造是由一个前进的拆离面引起的
IF 2.9 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-02-10 DOI: 10.1016/j.tecto.2026.231123
R.S. Chatterjee, Somalin Nath, Harsh Vatsa, G. Rawat, R.C. Patel, S.P. Mohanty, Rohit Kumar, Anush Kumar
Abstract
摘要
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引用次数: 0
Syn-convergent extension and deformation coupling in the Middle Mejerda basins (NW-Tunisia): Insights into polyphase evolution within the Tunisian orogenic wedge 突尼斯西北部Mejerda中部盆地同辐合伸展与变形耦合:对突尼斯造山带多期演化的认识
IF 2.9 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-02-04 DOI: 10.1016/j.tecto.2026.231112
Mohamed Sabri Arfaoui, Mohamed Gharbi
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引用次数: 0
P-wave seismic interferometric profile within the Granada Basin (Southern-Spain) 格拉纳达盆地(西班牙南部)纵波地震干涉剖面
IF 2.9 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-02-04 DOI: 10.1016/j.tecto.2026.231114
C. Araque-Pérez, D. Stich, T. Teixido, E. Carmona, J. Morales, F. Mancilla
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引用次数: 0
2D gravity modelling in Central Italy: Clues for the seismogenesis in the Apennines 意大利中部的二维重力模型:亚平宁山脉地震发生的线索
IF 2.9 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-02-04 DOI: 10.1016/j.tecto.2026.231113
M.M. Tiberti, M. Buttinelli, F.E. Maesano, F. Ferri, P. De Gori, L. Minelli, M. Di Nezza, C. D'Ambrogi
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引用次数: 0
Seismotectonics of the Panama Triple Junction region revealed by recent seismicity 近期地震活动揭示的巴拿马三合带地震构造
IF 2.6 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-02-03 DOI: 10.1016/j.tecto.2026.231115
Lepolt Linkimer, Ivonne G. Arroyo
The interaction among the Cocos, Nazca, and Panama plates at the Panama Triple Junction (PTJ) generates diverse seismic sources that remain poorly characterized. Using data from the National Seismological Network of Costa Rica and the Chirinet network of Panama, we analyzed four recent earthquake sequences (Mw 5.6–6.2, 2019–2021) near the Burica Peninsula and relocated 32 significant events (Mw 5.6–6.7) that occurred between 2000 and 2025. The results reveal: (1) right-lateral strike-slip faulting along the Panama and Balboa fracture zones; (2) right-lateral faulting on their inland projections, including the 2019 Mw 6.0 Canoas Fault earthquake; (3) reverse faulting during the 2008 (Mw 5.6) and 2020 (Mw 5.6) North Burica sequences, associated with the Media Fault Zone of the upper Panama Plate; (4) left-lateral strike-slip faulting within the subducting Cocos Plate, where at least five Mw 5.8–6.5 events occurred between 2002 and 2019; and (5) a seismogenic Cocos–Panama interplate zone extending southeast of the Burica Peninsula. We further reinterpret the 1934 Ms. 7.6 Armuelles tsunamigenic earthquake as a large megathrust rupture on this interplate boundary. Together, these findings refine the geometry of the seismic sources near the PTJ improving our understanding of the tectonic processes shaping the region.
Cocos、Nazca和巴拿马板块在巴拿马三重交界处(PTJ)的相互作用产生了各种各样的震源,这些震源的特征仍然很差。利用哥斯达黎加国家地震台网和巴拿马Chirinet网络的数据,我们分析了布里卡半岛附近最近发生的4次地震序列(Mw 5.6-6.2, 2019-2021),并重新定位了2000年至2025年间发生的32次重大地震事件(Mw 5.6-6.7)。结果表明:(1)巴拿马断裂带和巴尔博亚断裂带右侧走滑断裂;(2)右旋断层对其内陆投影的影响,包括2019年Mw 6.0 Canoas断层地震;(3)北布里卡层序2008年(Mw 5.6)和2020年(Mw 5.6)逆断裂,与上巴拿马板块介质断裂带有关;(4) Cocos板块内左侧走滑断裂,2002 - 2019年间至少发生5次Mw 5.8-6.5级地震;(5)布里卡半岛东南延伸的科科斯-巴拿马板块间带。我们进一步将1934年7.6 Ms. Armuelles海啸成因地震重新解释为该板块间边界上的大型逆冲断裂。总之,这些发现完善了PTJ附近震源的几何形状,提高了我们对塑造该地区的构造过程的理解。
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引用次数: 0
Significant stress variations in the West Pacific subduction zone derived from the summations of moment tensors of seismic events 西太平洋俯冲带的显著应力变化来源于地震事件矩张量的总和
IF 2.9 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-02-02 DOI: 10.1016/j.tecto.2026.231111
Xiubo Wang
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引用次数: 0
Mapping a proximal breakaway complex: Evidence of inherited basement fabric reactivation and polyphase rifting leading to the opening of a V-shaped basin at the Campos rifted margin proximal domain 近端断裂杂岩的定位:在坎波斯裂谷边缘近端域,继承的基底组构再活化和多相裂陷作用导致v型盆地张开的证据
IF 2.9 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-30 DOI: 10.1016/j.tecto.2026.231109
Aline Ribeiro, Natasha Stanton, Renata Schmitt, Andres Gordon, Pricilla Camões, Gwenn Peron-Pinvidic
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引用次数: 0
Deep multiparameter analysis of the precursory lithospheric, atmospheric and ionospheric anomalies before and during the 28 March 2025 Mw7.7 Myanmar-Burma earthquake 2025年3月28日Mw7.7缅甸-缅甸地震前后岩石圈、大气和电离层前兆异常的深度多参数分析
IF 2.9 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-30 DOI: 10.1016/j.tecto.2026.231101
Angelo De Santis, Xuemin Zhang, Saioa A. Campuzano, Pan Xiong, Gianfranco Cianchini, Jing Liu, Serena D'Arcangelo, Na Yang, Mariagrazia De Caro, Xinyan Ouyang, Martina Orlando, Maoning Feng, Loredana Perrone, Yongxian Zhang, Dario Sabbagh, Xinyi Jia, Maurizio Soldani, Hong Liu, Ariana Varela-Mendez
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引用次数: 0
Identification of the North Jining Basin Fault and its response to the northward expansion of the Shanxi rift system, North China 济宁盆地北断陷识别及其对山西裂谷系北扩的响应
IF 2.6 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-30 DOI: 10.1016/j.tecto.2026.231110
Zhikang Gong , Dongli Zhang , Weisheng Hou , Ting Liu , Jinhua Du , Haoyu Zhou , Zijian Feng , Xin Sun , Ruijie Xue , Haiyun Bi , Wenjun Zheng
The northward growth and expansion of the Shanxi rift system (SRS) are key to understanding the geodynamic evolution of the northeastern Ordos block. Previous studies have suggested that Shanxi rift activity weakens north of the Daihai–Huangqihai Basin under the influence of the EW-strike Zhangjiakou–Bohai tectonic zone. In this study, remote sensing and field investigations reveal an ∼100 km long prominent linear structure north of the Jining Basin in the northeastern Ordos block. Three high-density electrical resistivity tomography (ERT) profiles across this structure identify this region as the North Jining Basin Fault, NE-striking, SW-dipping normal fault that structurally controls the northern margin of the basin, exhibiting typical fault depression characteristics and latest activity in the Holocene. Geological evidence confirms that the fault offsets mid-Holocene sediments with a vertical displacement of ∼2.7 m. Combined with the spatiotemporal evolution of the Shanxi rift system, these findings suggest that the northeastern boundary of the rift remains active and continues to propagate northward, with the North Jining Basin Fault representing northward expansion of the extensional regime of the Shanxi rift.
山西裂谷系的北展发育是认识鄂尔多斯地块东北部地球动力学演化的关键。前人的研究认为,在东西向的张家口-渤海构造带的影响下,山西裂谷活动在岱海-黄旗海盆地以北减弱。在本研究中,通过遥感和野外调查,在鄂尔多斯地块东北部的济宁盆地北部发现了一条长约100 km的突出线性构造。3条高密度电阻率层析成像(ERT)剖面确定该地区为济宁盆地北断,北东向、西向正断层,构造上控制盆地北缘,具有典型断陷特征和全新世晚期活动。地质证据证实,该断层与中全新世沉积物的垂直位移为~ 2.7 m。结合山西裂谷系的时空演化特征,认为裂谷东北边界保持活跃并继续向北扩展,济宁盆地北断裂代表了山西裂谷伸展构造向北扩张。
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引用次数: 0
Deformation of the 1966 MW 7.1 Xingtai earthquake swarm in North China based on high-precision three-dimensional geodetic data 基于高精度三维大地测量资料的1966年华北地区mw7.1级邢台地震群形变
IF 2.9 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-01-28 DOI: 10.1016/j.tecto.2026.231097
Liu Chang, Yanqiang Wu, Wei Zhan, Yajin Pang, Nannan Guo, Guangli Su, Xiao Liu
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引用次数: 0
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Tectonophysics
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