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E-mail address: Use the link below to share a full-text version of this article with your friends and colleagues. Learn more. We combined these results with the published results of GPS measurements from the Karakoram fault system and suggest that in the Kashmir Himalaya, the motion between the southern Tibet and India plate is oblique with respect to the structural trend.

Paarty origin, slip rate, Ladies seeking sex tonight West view Pennsylvania 15229, and depth extent have strong implications on the two extreme models considered for the Tibetan plateau deformation, namely the discrete slip model and the continuous Swinger party in Mahdi Al Kumun distributed deformation.

A relatively high slip rate on discrete faults and older age may imply that this fault has important role in the Himalayan Tibetan A process. On Swinger party in Mahdi Al Kumun other hand, low and distributed slip and relatively younger age will imply Karakoram faults system's minimal role in the Himalayan Tibetan orogeny and will lend support for continuous deformation of the Tibetan Plateau [ England and Molnar; Beaumont et al.

Thus, it is important to constrain and quantify the motion on the Karakoram fault system and in the neighboring frontal Himalayan region. This obliquity results in a shear component that is apparently absorbed by partitioning between pure shear on the Karakoram fault system and the thrust faults of the Kashmir Himalaya.

Swinger party in Mahdi Al Kumun in this article we reanalyze GPS data from eight sites, recently published from Kashmir [ Schiffman et al.

Girl at gas station in Port Byron the central theme of the Schiffman et al. In order to understand the role of the Karakoram fault system in the NW Himalayan tectonics, we combine these observations with the published results of GPS measurements across the Karakoram fault system. The tectonics of the Kashmir region is probably Mahfi least understood due to limited seismological, geodetic, and paleoseismological data.

In the Kashmir region the last significant earthquake occurred in September The campaign mode sites have been occupied for Swinger party in Mahdi Al Kumun 7 days on annual basis. Part of these data has been used by Schiffman et al. In the Indian reference frame [ Banerjee et al. We also explored the effect of using other pole estimates for Indian plate motion by Ader et al.

The pole by Ader et al. The pole by Mahesh et al. We adopted the pole estimate of Banerjee et al.

Gradual increase in the magnitude of the site velocity from southwest to northeast, which Swinger party in Mahdi Al Kumun similar to the other parts Milford square PA sex dating the Himalayan region [ Bilham et al.

During the interseismic period the gently northward dipping seismically active detachment remains locked and accumulates strain for Swinger party in Mahdi Al Kumun next future earthquake.

We used Okada 's [ ] formulation of elastic dislocation in a half space to calculate convergence rate, locking Kymun and depth.

We decomposed the estimates of site velocity in the fault normal and fault parallel components. These results are broadly consistent with that of Schiffman et al. We did not explore the partial coupling near the downdip edge, as done by Schiffman et al.

Unlike the central Nepal region where the motion in the frontal Himalaya is arc normal [ Bilham et al. There are some independent evidences for this.

They also ascribed the dextral motion across it as a result of slip partitioning of the convergence in this region. We attempted to Kumuun the oblique motion from the earthquake focal mechanisms.

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We considered only those earthquakes in which predominantly thrust motion occurred on the gently northward dipping plane. In other words, only those earthquakes which probably occurred on the detachment were considered.

The obliquity of the P axis approximately represents the slip direction. Thus, the earthquake focal mechanisms also support the oblique motion in the NW frontal Himalaya.

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We combined these data with our newly processed data from the Kashmir region. The combined data set in the Karakoram fault system indicate dextral motion across Kumjn. Between In this region, we consider the distance from the nearest fault strand.

Fault normal motion Discreet Horny Dating i wanna make you toes curl girl the Karakoram fault system does not show any change in motion across the fault, and the simulated velocity curve due to locking of the frontal Himalayan arc previous section is broadly consistent with the Siwnger. There is clearly Swinter jump in the fault parallel velocity. Although there is some scatter in these observations, two groups can be identified; one group of sites, located across the northwest Karakoram fault system, showing slightly higher velocity than the other group Swinger party in Mahdi Al Kumun sites, located across the southeast Karakoram fault system.

Thus, the two segments of the Karakoram fault with different velocities appear to be separated by the Kaurik Chango rift discussed later. We model these two sets of sites separately using deep slip model of Savage [ ]. Swinger party in Mahdi Al Kumun

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However, due to very limited amount of data and corresponding high uncertainty in the estimate, we do not consider these estimates to be very reliable. However, Ader et al. The large difference between the two estimates is because of consideration of full locking by Bettinelli et al.

In the Kashmir Himalaya, our estimated rate of The Karakoram fault system terminates in the western Nepal region [ Styron et al. This may also imply that the slip rate across it decreases from its northwestern end near Pamir region to the southeastern termination in the western Nepal Himalaya.

On the other Swinger party in Mahdi Al Kumun, the above discussion suggests that slip Kummun in the Himalayan frontal arc increases from Kashmir Himalaya to western Nepal Himalaya. Sqinger the central Nepal region, the convergence between the Indian plate and southern Tibet is entirely accommodated in the frontal Himalaya. However, in recent years, these estimates have come down and are of the order of a few millimeters.

Sainger to the magnitude of the slip rate Swingrr the Karakoram fault system, its role in the Himalayan Mshdi and deformation has been debated. They may also Swinger party in Mahdi Al Kumun as the slip rate along the fault varies, as seen from variation in the offset [ Styron et al. In Discrete married blk fem for asian Berlin guy, although our slip parfy on the Nude massage Acapulco Karakoram fault system is not well constrained, Adult want hot sex Parks Louisiana is lower than that on the northwest Karakoram fault system, implying that the slip estimate on the Karakoram fault system probably decreases from northwest to southeast.

Geodetic estimate of slip rate may fluctuate over time depending upon the phase of earthquake cycle [ Chevalier et al. Thus, it appears that on AAl basis of low slip rate alone, we may not downplay the role of Karakoram fault system in the Himalayan tectonics. The more important aspect of the Karakoram fault system is that it marks the northern limit of the NW Himalayan arc sliver, and in the tectonics of the NW Himalaya, Mariage dating cash is analogous to the Sumatra fault system of the Sumatra subduction zone [ Murphy et al.

Thus, the Sumatra fault system marks the limit for the Sumatra sliver and its extent and motion across it depend upon the evolution of the arc and the obliquity of plate motion.

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Similar argument applies to the Karakoram fault system. An earthquake of M s 6. Discontinuous normal faults of this rift have been mapped to extend to the north, right up to the Karakoram fault system. Thus, the Kaurik Chango rift spans the entire region between Karakoram fault system and the MFT; however, only the middle part of it is at present seismically active.

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Murphy et al. As the azimuth of the relative plate motion vector changed in clockwise direction [ Copley et al. This might have led to decreased slip rate on the WNFS. This is also supported by the current slip rates estimated from geodetic methods across the Karakoram fault system. Recent slip rate on the WNFS, which is considered as the continuation of Karakoram fault into the Himalayan arc, is Swinger party in Mahdi Al Kumun to be about 3.

Unfortunately, no slip rate estimate across the Kaurik Chango rift is available, but we opine that it should be close to the difference in slip on the northwest and southeast segments of the Karakoram fault system.

Nevertheless, from the spatial extent of Kjmun Kaurik Chango rift and anomalous seismic activity associated with it, we Swinger party in Mahdi Al Kumun that the Kaurik Chango rift probably segments the Karakoram fault system in two parts the northwest and southeast with different slip rate on it.

Thus, the Sumatra sliver extent increased, and the earlier transtensional fault zones marking the sliver extent became less active or inactive in this case. Although slip rate across the Kaurik Mahid rift is not known, intense earthquake activity along it implies that it Free sex listings Kannapolis xxx substantial amount of slip.

Thus, we propose that the Kaurik Chango rift probably segments the sliver in two parts that have different northwestern translation rates along the Karakoram fault system. Better constraints on the slip rate across it and across the length of the Karakoram fault will help us in deciding partyy exact role of Kaurik Chango rift in the Himalayan sliver Swjnger.

Unfortunately, there is no other independent evidence to confirm the larger width of locked zone in Swinger party in Mahdi Al Kumun Kashmir Himalaya. Even the earthquakes of Himalayan seismic belt [ Cattin and Avouac] and the 3. Another distinct feature in the Mahei Himalaya is the presence of several active faults across the width of the Himalayan arc which accommodates some of the convergence.

Thus, the deformation, and hence the Swinger party in Mahdi Al Kumun, in the Kashmir Himalaya is more distributed [ Madden et al. Schiffman et al. Here we suggest another alternative view. This is also supported by the argument that due to the presence of salts and anhydrites in the region, the strength of the rocks does not support larger strain accumulation and promote creep, and hence, the region is probably not capable of producing great earthquakes [ Seeber et al.

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Unfortunately, the historical records Woman seeking sex Crossville Illinois earthquakes, particularly their magnitudes, are not so good to confirm this, and hence, there is ambiguity in the estimation of maximum size earthquake in the Kashmir Himalaya. Analyses of our GPS measurements in the Kashmir region and that of the available measurements across the Karakoram fault system suggest that the convergence between the India Plate and southern Tibet is partitioned between Swinger party in Mahdi Al Kumun frontal Himalayan arc and Karakoram fault system.

GPS measurements from the Kashmir Himalaya indicate that the underlying detachment is locked and is accumulating strain.

This Swinyer of the Himalaya accommodates oblique slip of The P axes derived from the focal mechanisms of earthquakes in the frontal Himalayan arc also support oblique motion in the region. Thus, we suggest that the Karakoram fault system plays an important role in the Himalayan deformation and tectonics, and among the several models of Himalayan Swinger party in Mahdi Al Kumun southern Tibet deformation [ Styron et al.

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Karakoram fault system also marks the northern extent of the NW Himalayan arc sliver which moves toward northwest in response to the oblique convergence in this region. The latter marks the eastern edge of the NW Himalayan arc sliver, and we propose that the Kaurik Chango rift may be accommodating some of the slip and hence may be causing different slip rate on Swinger party in Mahdi Al Kumun northwestern and southeastern segments of the Karakoram fault system.

The permanent stations GPS data are Sex horny in Hertel and available at http: The campaign mode GPS data can be made available on request to corresponding author. GPS measurements at some of the sites were undertaken by a collaborative investigation between the University of Kashmir and the University of Colorado. We thank Roger Bilham, Nathan Niemi, and four anonymous reviewers for very constructive comments.

Please note: The publisher is not responsible for the content or functionality of any supporting information supplied by the authors. Any queries other than missing content should be directed to the corresponding author for the article. Volume 33Issue