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Riasi Fault

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Journal Article
Journal: GSA Bulletin
Published: 01 July 2016
GSA Bulletin (2016) 128 (7-8): 1070–1094.
...Y. Gavillot; A. Meigs; D. Yule; R. Heermance; T. Rittenour; C. Madugo; M. Malik Abstract New mapping demonstrates that active emergent thrust faulting is occurring within the fold-and-thrust belt north of the deformation thrust front in the NW Himalaya. The >60-km-long Riasi fault system...
FIGURES | View All (14)
Image
<span class="search-highlight">Riasi</span> <span class="search-highlight">Fault</span>, Murree Formation (A) thrusted over Dhok Pathan Formation (B) n...
Published: 01 December 2013
Photo 7. Riasi Fault, Murree Formation (A) thrusted over Dhok Pathan Formation (B) near Chauki area (Station NS-4; Plate 2), Photograph facing southeast. Note: The shearing and crushing is present along the fault.
Image
Drag folds associated with <span class="search-highlight">Riasi</span> <span class="search-highlight">fault</span> near Sarhota (Station SC-1; Plate 2)...
Published: 01 December 2013
Photo 8. Drag folds associated with Riasi fault near Sarhota (Station SC-1; Plate 2). Photo facing southeast
Image
Regional cross section along SW-NE transect shown in  Figures 1  and  2 . S...
Published: 01 July 2016
Figure 13. Regional cross section along SW-NE transect shown in Figures 1 and 2 . Shown are summary results of geological shortening rates for the Riasi fault system and frontal folds, including the Suruin-Mastgarh anticline. For more detailed explanation of cross section constraints
Journal Article
Published: 01 January 2024
Jour. Geol. Soc. India (2024) 100 (1): 78–90.
... Syntaxis is its antiformality. The project area is bounded to the east by the Riasi fault and to the west by the Jhelum fault, while to the south it is bounded by Salt Range Thrust. Research is being conducted in the areas of Narmah, Sahan, Pirgali, Kas Guma, Mohra Jangu, and Kalri. Fold-and-thrust belts...
FIGURES | View All (14)
Journal Article
Published: 01 January 2018
Jour. Geol. Soc. India (2018) 91 (1): 57–66.
... areas of Rawalpindi and Sudhnoti districts. The southeastern limb of the Hazara Kashmir syntaxis is imbricated along Punjal thrust, Main Boundary thrust and Riasi fault. The Jhelum fault truncates the western limb of Hazara Kashmir syntaxis. The core of syntaxis comprises of Himalayan molasse deposits...
FIGURES | View All (12)
Journal Article
Published: 01 December 2013
Jour. Geol. Soc. India (2013) 82 (6): 639–648.
...Photo 7. Riasi Fault, Murree Formation (A) thrusted over Dhok Pathan Formation (B) near Chauki area (Station NS-4; Plate 2), Photograph facing southeast. Note: The shearing and crushing is present along the fault. ...
FIGURES | View All (18)
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Regional geologic map of the Kashmir Himalaya (modified after  Ranga Rao an...
Published: 01 July 2016
—Balapora fault; RF—Riasi fault system; MKT—Mandili-Kishanpur thrust; MT—Mudun thrust; TT—Tanhal thrust; SMA—Suruin-Mastgarh anticline. See Figure 13 for cross section.
Image
Topographic map of the Jammu and Kashmir Himalaya showing the meisoseismal ...
Published: 18 March 2020
, Balakot‐Bagh fault; BF, Balpora fault; GCT, Great Counter thrust; KT, Kotli thrust; KW, Kishtwar Window; MKT, Mandli‐Kishanpur thrust; RF, Riasi fault; SRT, Salt Range thrust; and ZSZ, Zanskar shear zone. The major cities of Srinagar and Jammu are plotted as squares. The color version of this figure
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Regional structure map of the Himalaya thrust belt in northwest India and P...
Published: 01 July 2016
—Zanskar shear zone; KW—Kishtwar window; RW—Rampur window; MCT—Main Central thrust; MBT—Main Boundary thrust; BF—Balapora fault; BBF—Balakot-Bagh fault; KT—Kotli thrust; RF—Riasi fault system; MKT—Mandili-Kishanpur thrust; JT—Jawalamukhi thrust; ST—Soan thrust; JA—Janauri anticline; HFT—Himalayan Frontal
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Interpretative model for the sequence of deformation for the offset Bidda t...
Published: 01 July 2016
Figure 14. Interpretative model for the sequence of deformation for the offset Bidda terrace and underlying Qcc unit. In model, (A) Main Riasi thrust (MRT) and its southern fault splay Frontal Riasi thrust (FRT) formed prior to 100 ka, with the same present-day fault geometry. (B) At ca. 100 ka
Journal Article
Published: 01 March 2024
Jour. Geol. Soc. India (2024) 100 (3): 459.
... sector of NW Himalaya. The Hazara-Kashmir Syntaxis runs through numerous areas within Mirpur district. One of the key characteristics of the Hazara-Kashmir Syntaxis is its antiformality. The project area is bounded to the east by the Riasi fault and to the west by the Jhelum fault, while to the south...
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Soil profiles (above) and landscape interpretation diagram (below) across t...
Published: 01 July 2016
Figure 11. Soil profiles (above) and landscape interpretation diagram (below) across the Frontal Riasi thrust (FRT) and surface T3 (Dugalla terrace) for pits 1–4 (see Fig. 6 for soil pit locations). Brown-red silt and gravel characterize the upper soil horizons in the hanging wall (pit 1
Journal Article
Published: 01 June 1973
Jour. Geol. Soc. India (1973) 14 (2): 190–193.
... is of this type (Kingsley, 1931). Here the noncommittal term 'ring fracture' is used in preference to 'ring fault' because there are no convincing field evidences which could indicate that the quartz porphyry ring dyke occupied a ring fault, but for the presence of a fault scarp on the eastern side of the hill...
Journal Article
Published: 01 April 1990
Jour. Geol. Soc. India (1990) 35 (4): 390–394.
... by the orogenic movement during Quaternary period which resulted in the evolution of present-day landscape. EVIDENCES OF QUATERNARY TECTONICS IN SIWALIKS Evidences of Quaternary tectonics are documented from Siwaliks of Pakistanand parts of India. The evidences of faults cutting across the post-Siwalik...
Journal Article
Published: 01 March 1970
Jour. Geol. Soc. India (1970) 11 (1): 90–96.
... to the Agglomeratic Sl~tes) which occur underneath the Limestones of Kotli 'inlier' assigned a Permian 94 DISCUSSION age to these bodies. There are indications that these slates occurring confined to faulted isoclinal-synclines within the Riasi Limestones are not possibly part of Agglomeratic Slate group, and hence...
Journal Article
Published: 01 November 1991
Jour. Geol. Soc. India (1991) 38 (5): 516–523.
...B. K. Nayak; Rajesh Sharma Abstract A strong stratigraphic control is exhibited by the sporadic Pb-Zn occurrences in the Great Limestone of Riasi, J & K. Fluid inclusion thermometry and stable isotope data suggest their remobilisation and concentration in the fractures developed in the host...
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The Kashmir Himalaya is located at the junction of Indian and Eurasian plat...
Published: 01 November 2023
thrust and active regional faults over the Kashmir Himalaya (from Dasgupta et al., 2000 ) are IKSZ (Indus-Kohistan Seismic Zone), ISZ (Indus-Suture Zone), MCT (Main Central Thrust), MBT (Main Boundary Thrust), and all other shown regional faults (Balapore, Bagh Balakot, Riasi Thrust, Jhelum, Mangala
Journal Article
Published: 01 May 1978
Jour. Geol. Soc. India (1978) 19 (5): 221–223.
... to faulting (Raha, 1976). However, the LOCC1fion of qoleno in Jammu L imeston. Figure I. Map showing location of galena in the Riasi inlier of the Limestone (inset location of the area ). base of the formation is not exposed anywhere and it is unconformably overlain by the Eocene Subathu Formation wbich...
Journal Article
Published: 01 September 1970
Jour. Geol. Soc. India (1970) 11 (3): 288–302.
... embayments of the Krol and older rocks, and the whole complex had been subsequently folded and submitted to minor reversed faulting, it would have been expected that the Nummulitics would generally have the same formation above and below as that against which it had originally been deposited. Yet...