|
|
|
篇目详细内容 |
|
【篇名】 |
Tectonic control on the drainage system in a piedmont region in tectonically active eastern Himalayas |
|
【刊名】 |
Frontiers of Earth Science |
|
【刊名缩写】 |
Front. Earth Sci |
|
【ISSN】 |
2095-0195 |
|
【EISSN】 |
2095-0209 |
|
【DOI】 |
10.1007/s11707-012-0297-z |
|
【出版社】 |
Higher Education Press and Springer-Verlag Berlin
Heidelberg |
|
【出版年】 |
2012 |
|
【卷期】 |
6
卷1期 |
|
【页码】 |
29-38
页,共
10
页 |
|
【作者】 |
Chandreyee GOSWAMI;
Dhruba MUKHOPADHYAY;
Bikash Chandra PODDAR;
|
|
【关键词】 |
alluvial fan; drainage pattern; thrust; normal fault; active tectonic |
【摘要】 |
|
The impact of neotectonic activity on drainage system has been studied in a large alluvial fan in the eastern Himalayan piedmont area between the Mal River and the Murti River. Two distinct E–W lineaments passing through this area had been identified by Nakata (1972, 1989) as active faults. The northern lineament manifested as Matiali scarp and the southern one manifested as Chalsa scarp represent the ramp anticlines over two blind faults, probably the Main Boundary Thrust (MBT) and the Himalayan Frontal Thrust (HFT), respectively. The fan surface is folded into two antiforms with a synform in between. These folds are interpreted as fault propagation folds over the two north dipping blind thrusts. Two lineaments trending NNE–SSW and nearly N–S, respectively, are identified, and parts of present day courses of the Murti and Neora Rivers follow them. These lineaments are named as Murti and Neora lineaments and are interpreted to represent a conjugate set of normal faults. The rivers have changed their courses by the influence of these normal faults along the Murti and Neora lineaments and their profiles show knick points where they cross E–W thrusts. The overall drainage pattern is changed from radial pattern in north of the Matiali scarp to a subparallel one in south due to these conjugate normal faults. The interfluve area between these two rivers is uplifted as a result of vertical movements on the above mentioned faults. Four major terraces and some minor terraces are present along the major river valleys and these are formed due to episodic upliftment of the ground and subsequent downcutting of the rivers. The uppermost terrace shows a northerly slope north of the Chalsa scarp as a result of folding mentioned above. But rivers on this terrace form incised channels keeping their flow southerly suggesting that they are antecedent to the folding and their downcutting kept pace with the tectonism. |
|
