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1-20 OF 42 RESULTS FOR
Riasi Fault
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Journal Article
Shortening rate and Holocene surface rupture on the Riasi fault system in the Kashmir Himalaya: Active thrusting within the Northwest Himalayan orogenic wedge
Journal: GSA Bulletin
Publisher: Geological Society of America
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...
Image
Riasi Fault, Murree Formation (A) thrusted over Dhok Pathan Formation (B) n...
in Stratigraphy and Structure of Sarda, Manil, Changpur and Naghal Areas, District Kotli, Jammu & Kashmir
> Journal of the Geological Society of India
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 Riasi fault near Sarhota (Station SC-1; Plate 2)...
in Stratigraphy and Structure of Sarda, Manil, Changpur and Naghal Areas, District Kotli, Jammu & Kashmir
> Journal of the Geological Society of India
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...
in Shortening rate and Holocene surface rupture on the Riasi fault system in the Kashmir Himalaya: Active thrusting within the Northwest Himalayan orogenic wedge
> GSA Bulletin
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
Structural and Stratigraphic Study of Hazara-Kashmir Syntaxis with the Aid of Geographic Information System and Field Data Approach
Publisher: Geological Society of India
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...
Journal Article
Structure and Stratigraphy of Rumbli and Panjar Areas of Kashmir and Pakistan with the Aid of GIS
Publisher: Geological Society of India
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...
Journal Article
Stratigraphy and Structure of Sarda, Manil, Changpur and Naghal Areas, District Kotli, Jammu & Kashmir
Publisher: Geological Society of India
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. ...
Image
Regional geologic map of the Kashmir Himalaya (modified after Ranga Rao an...
in Shortening rate and Holocene surface rupture on the Riasi fault system in the Kashmir Himalaya: Active thrusting within the Northwest Himalayan orogenic wedge
> GSA Bulletin
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 ...
in A Report on Broadband Seismological Experiment in the Jammu and Kashmir Himalaya (JAKSNET)
> Seismological Research Letters
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
Image
Regional structure map of the Himalaya thrust belt in northwest India and P...
in Shortening rate and Holocene surface rupture on the Riasi fault system in the Kashmir Himalaya: Active thrusting within the Northwest Himalayan orogenic wedge
> GSA Bulletin
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
Image
Interpretative model for the sequence of deformation for the offset Bidda t...
in Shortening rate and Holocene surface rupture on the Riasi fault system in the Kashmir Himalaya: Active thrusting within the Northwest Himalayan orogenic wedge
> GSA Bulletin
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
Structural and Stratigraphic Study of Hazara-Kashmir Syntax, Pakistan with the Aid of Geographic Information System and Field Data Approach
Publisher: Geological Society of India
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...
Image
Soil profiles (above) and landscape interpretation diagram (below) across t...
in Shortening rate and Holocene surface rupture on the Riasi fault system in the Kashmir Himalaya: Active thrusting within the Northwest Himalayan orogenic wedge
> GSA Bulletin
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
On the Occurrence of a Ring Dyke in the Tusham Igneous Complex, Hissar (Haryana)
Publisher: Geological Society of India
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
Late Pleistocene Fluvial Response to Tectonics in Jammu, Jammu and Kashmir
Publisher: Geological Society of India
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
Discussion
Publisher: Geological Society of India
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
Syn-Sedimentary and Later Remobilised Epithermal Pb-Zn Mineralisation of the Great Limestone, Riasi, J & K - Signatures in Fluid Inclusions and Stable Isotope Compositions
Publisher: Geological Society of India
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...
Image
The Kashmir Himalaya is located at the junction of Indian and Eurasian plat...
in Site response analysis beneath the Kashmir basin (NW Himalaya) using ambient noise
> Earthquake Spectra
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
Geochronology of the Jammu Limestone, Udhampur District, Jammu & Kashmir State, India
Publisher: Geological Society of India
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
Discussion
Publisher: Geological Society of India
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...
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