scholarly article | Q13442814 |
P819 | ADS bibcode | 2002Tecto..21.1062D |
P356 | DOI | 10.1029/2001TC001322 |
P50 | author | Peter G. DeCelles | Q64729706 |
P2093 | author name string | George Zandt | |
Delores M. Robinson | |||
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Palaeomagnetic estimates of crustal shortening in the Himalayan thrusts and Zangbo suture | Q56566437 | ||
Paleogeographic maps of the continents bordering the Indian Ocean since the Early Jurassic | Q56566438 | ||
The Himalayan passive margin from Precambrian to Cretaceous times | Q56566440 | ||
The Himalayan Arc: large-scale continental subduction, oroclinal bending and back-arc spreading | Q56566449 | ||
Kinematics, topography, shortening, and extrusion in the India-Eurasia collision | Q56566450 | ||
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Structural evolution and sequence of thrusting in the High Himalayan, Tibetan—Tethys and Indus suture zones of Zanskar and Ladakh, Western Himalaya | Q56673550 | ||
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How flat is Tibet? | Q58472171 | ||
Normal faulting in central Tibet since at least 13.5 Myr ago | Q59038463 | ||
Diachronous uplift of the Tibetan plateau starting 40 Myr ago | Q59053343 | ||
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Implications of crustal property variations for models of Tibetan plateau evolution | Q59056199 | ||
Evidence for Tibetan plateau uplift before 14 Myr ago from a new minimum age for east–west extension | Q59058630 | ||
Timing of Tibetan uplift constrained by analysis of volcanic rocks | Q59058647 | ||
Cordilleran Benioff zones | Q59065356 | ||
Himalayan tectonics explained by extrusion of a low-viscosity crustal channel coupled to focused surface denudation | Q59068319 | ||
The Tibetan side of the India–Eurasia collision | Q59069417 | ||
Seismic anisotropy as an indicator of mantle flow beneath the Himalayas and Tibet | Q59072758 | ||
GPS measurements of present-day convergence across the Nepal Himalaya | Q59091590 | ||
Structure and evolution of the Himalaya–Tibet orogenic belt | Q59092453 | ||
Propagating extrusion tectonics in Asia: New insights from simple experiments with plasticine | Q59238938 | ||
Thrust tectonics and the deep structure of the Pakistan Himalaya | Q59608740 | ||
Records of the evolution of the Himalayan orogen from in situ Th–Pb ion microprobe dating of monazite: Eastern Nepal and western Garhwal | Q59791058 | ||
Lithospheric structure of the Qiangtang Terrane, northern Tibetan Plateau, from complete regional waveform modeling: Evidence for partial melt | Q59797271 | ||
Detection of Widespread Fluids in the Tibetan Crust by Magnetotelluric Studies | Q59835786 | ||
Seismic anisotropy beneath Tibet: evidence for eastward extrusion of the Tibetan lithosphere? | Q59853895 | ||
Active thrusting and folding in the Qilian Shan, and decoupling between upper crust and mantle in northeastern Tibet | Q59853987 | ||
Mountain belts and the new global tectonics | Q60568849 | ||
Southward extrusion of Tibetan crust and its effect on Himalayan tectonics | Q60635334 | ||
Present-Day Crustal Deformation in China Constrained by Global Positioning System Measurements | Q60709883 | ||
Kinematics of the India-Eurasia collision zone from GPS measurements | Q60709891 | ||
Crustal structure of central Tibet as derived from project INDEPTH wide-angle seismic data | Q60710432 | ||
Seismic Images of Crust and Upper Mantle Beneath Tibet: Evidence for Eurasian Plate Subduction | Q60719224 | ||
Lithostratigraphic correlations in the western Himalaya—An isotopic approach | Q64025209 | ||
Age and composition of dikes in Southern Tibet: New constraints on the timing of east-west extension and its relationship to postcollisional volcanism | Q64447168 | ||
A Review of Geophysical Constraints on the Deep Structure of the Tibetan Plateau, the Himalaya and the Karakoram, and their Tectonic Implications | Q69672460 | ||
Intracrustal subduction and gravity currents in the deep crust: Sm-Nd, Ar-Ar, and thermobarometric constraints from the Skagit Gneiss Complex, Washington | Q70050005 | ||
Surface Deformation and Lower Crustal Flow in Eastern Tibet | Q73257755 | ||
Tectonic implications of U-Pb zircon ages of the himalayan orogenic belt in nepal | Q73698422 | ||
When did the roof collapse? Late Miocene north-south extension in the high Himalaya revealed by Th-Pb monazite dating of the Khula Kangri granite | Q78909430 | ||
Raising tibet | Q80929428 | ||
Trench-parallel flow beneath the nazca plate from seismic anisotropy | Q81182361 | ||
Tectonostratigraphic model for underfilled peripheral foreland basins: An Alpine perspective | Q96411273 | ||
Active folding of fluvial terraces across the Siwaliks Hills, Himalayas of central Nepal | Q96776859 | ||
Himalayan metamorphic sequence as an orogenic channel: insight from Bhutan | Q97323294 | ||
Evolutionary model of the Himalaya–Tibet system: geopoembased on new modelling, geological and geophysical data | Q97323427 | ||
Stratigraphy, structure, and tectonic evolution of the Himalayan fold-thrust belt in western Nepal | Q97323495 | ||
Tectonics of the Himalaya and southern Tibet from two perspectives | Q97448065 | ||
Neotectonics of the Min Shan, China: Implications for mechanisms driving Quaternary deformation along the eastern margin of the Tibetan Plateau | Q97448066 | ||
Mode of Cenozoic east-west extension in Tibet suggesting a common origin of rifts in Asia during the Indo-Asian collision | Q97448092 | ||
Initiation and Long-Term Slip History of the Altyn Tagh Fault | Q97448151 | ||
Fault plane solutions of earthquakes and active tectonics of the Tibetan Plateau and its margins | Q97449153 | ||
Post-Collisional Potassic and Ultrapotassic Magmatism in SW Tibet: Geochemical and Sr-Nd-Pb-O Isotopic Constraints for Mantle Source Characteristics and Petrogenesis | Q97449230 | ||
Injection of Indian crust into Tibetan lower crust: A two-dimensional finite element model study | Q97449290 | ||
Quaternary extension in southern Tibet: Field observations and tectonic implications | Q97449339 | ||
Palaeomagnetism of Cretaceous to Tertiary sediments from southern Tibet: evidence for the extent of the northern margin of India prior to the collision with Eurasia | Q97449449 | ||
Mapping the descent of Indian and Eurasian plates beneath the Tibetan Plateau from gravity anomalies | Q97449456 | ||
STRUCTURE OF THE SIWALIKS OF WESTERN NEPAL: AN INTRACONTINENTAL ACCRETIONARY PRISM | Q97449471 | ||
Lateral extrusion of lower crust from under high topography in the isostatic limit | Q97484821 | ||
Focal depths and fault plane solutions of earthquakes under the Tibetan Plateau | Q97488333 | ||
Upper mantle velocity structure beneath the Tibetan Plateau from Pn travel time tomography | Q98969146 | ||
Mechanics of fold-and-thrust belts and accretionary wedges | Q101831016 | ||
Shear wave splitting, continental keels, and patterns of mantle flow | Q104200341 | ||
Slab breakoff: A model of lithosphere detachment and its test in the magmatism and deformation of collisional orogens | Q104385337 | ||
Isotope geochemistry of the 1985 Tibet Geotraverse, Lhasa to Golmud | Q104414117 | ||
High times on the Tibetan Plateau: Paleoelevation of the Thakkhola graben, Nepal | Q104776784 | ||
The kinematic evolution of the Nepalese Himalaya interpreted from Nd isotopes | Q104795803 | ||
Tectonic history of the Altyn Tagh fault system in northern Tibet inferred from Cenozoic sedimentation | Q106115737 | ||
Topographic ooze: Building the eastern margin of Tibet by lower crustal flow | Q106999429 | ||
P433 | issue | 6 | |
P304 | page(s) | 12-1-12-25 | |
P577 | publication date | 2002-12-01 | |
P1433 | published in | Tectonics | Q15766817 |
P1476 | title | Implications of shortening in the Himalayan fold-thrust belt for uplift of the Tibetan Plateau | |
P478 | volume | 21 |
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Q97337337 | Comparisons of the kinematics and deep structures of the Zagros and Himalaya and of the Iranian and Tibetan plateaus and geodynamic implications |
Q106464998 | Crustal channel flows: 1. Numerical models with applications to the tectonics of the Himalayan-Tibetan orogen |
Q106465000 | Crustal channel flows: 2. Numerical models with implications for metamorphism in the Himalayan-Tibetan orogen |
Q41109460 | Crustal rheology controls on the Tibetan plateau formation during India-Asia convergence |
Q107214449 | Effect of unbalanced topography and overloading on Coulomb wedge kinematics: Insights from sandbox modeling |
Q101072393 | Eocene porphyry copper deposits in the eastern Tibetan Plateau, China: Uplift, denudation, and implications for mineral exploration |
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Q97448009 | Heterogeneity and anisotropy of the lithosphere of SE Tibet from surface wave array tomography |
Q60710385 | Injection of Tibetan crust beneath the south Qaidam Basin: Evidence from INDEPTH IV wide-angle seismic data |
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Q59794630 | Mesozoic and Cenozoic tectonic evolution of the Shiquanhe area of western Tibet |
Q97337341 | Middle to late Miocene extremely rapid exhumation and thermal reequilibration in the Kung Co rift, southern Tibet |
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Q59794617 | Nyainqentanglha Shan: A window into the tectonic, thermal, and geochemical evolution of the Lhasa block, southern Tibet |
Q56566446 | Paleocene-Eocene record of ophiolite obduction and initial India-Asia collision, south central Tibet |
Q94589757 | Rates of late Quaternary normal faulting in central Tibet from U-series dating of pedogenic carbonate in displaced fluvial gravel deposits |
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