Shuttle 发表于 2025-3-23 10:51:31
Observation of Organic Nature (A)seismic reflection/ refraction profiles as well as gravity and thermal studies carried out in the foredeep area of the southern and eastern Carpathians provide information on the crustal structure of the study region. The variability in the reflectivity pattern and crustal thickness shown by the difjaundiced 发表于 2025-3-23 15:17:40
http://reply.papertrans.cn/19/1810/180935/180935_12.png量被毁坏 发表于 2025-3-23 21:38:06
https://doi.org/10.1007/978-94-015-0670-0ize, increased sharpness with depth, asymmetry, and association with faulting. These folds are ascribed to the compaction of sediments over crystalline, rigid basement, in this instance tilted Precambrian fault blocks. Initially, the ‘plains-type folds’ were formed when the present major structural馆长 发表于 2025-3-23 23:28:41
https://doi.org/10.1007/978-94-009-1598-5Deformation; correlation; fault; orogenic belt; orogeny; plate tectonics; tectonics; structural geology吞噬 发表于 2025-3-24 02:22:36
http://reply.papertrans.cn/19/1810/180935/180935_15.png演绎 发表于 2025-3-24 09:49:47
http://reply.papertrans.cn/19/1810/180935/180935_16.pngcortisol 发表于 2025-3-24 13:15:01
0928-267X the first time that a meeting of this series took place in the centre of Europe and the first such meeting in this area after the recent political changes in eastern Europe. Consequently, the main theme of the meeting focussed on the structure and history of the entire European continent. Further th易受骗 发表于 2025-3-24 18:37:25
http://reply.papertrans.cn/19/1810/180935/180935_18.pngBombast 发表于 2025-3-24 20:32:13
Observation of Organic Nature (A) are best described as measures (or fields). This paper presents a multifractal method for describing crack and fault patterns in rocks using computer images of crack (fault) clusters and fault systems as depicted on geologic maps.OATH 发表于 2025-3-25 01:59:06
Multifractal Analysis of Fault Structures in Basement Rocks are best described as measures (or fields). This paper presents a multifractal method for describing crack and fault patterns in rocks using computer images of crack (fault) clusters and fault systems as depicted on geologic maps.