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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Upper Carboniferous (2)
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upper Precambrian
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volcanic rocks
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phosphates
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framework silicates
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plagioclase
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silica minerals
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orthosilicates
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datolite group
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majorite (1)
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zircon group
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zircon (30)
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sorosilicates
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epidote group
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ring silicates
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emerald (3)
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tourmaline group
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schorl (2)
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sheet silicates
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mica group
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serpentine group
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talc (1)
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sulfates (1)
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wehrlite (1)
-
-
Primary terms
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absolute age (54)
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Arctic region
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Svalbard
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Asia
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Arabian Peninsula
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Central Asia
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Far East
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China
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Indonesia
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Lesser Himalayas (4)
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Nanga Parbat (26)
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Zanskar Range (10)
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Hindu Kush (5)
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Indian Peninsula
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India
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Simla Hills (1)
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Spiti (2)
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Rajasthan India
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Aravalli Range (1)
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Sikkim India (1)
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Indian Shield (1)
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Indo-Gangetic Plain (1)
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Indus Basin (4)
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Indus Valley (5)
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Jammu and Kashmir
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Azad Kashmir Pakistan (7)
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Jammu (5)
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Kashmir (26)
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Kashmir Valley (3)
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Ladakh (50)
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Kohistan (26)
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Swat Pakistan (2)
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Punjab Pakistan
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Attock Pakistan (1)
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Mangla Dam (3)
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Mansehra Pakistan (1)
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Salt Range (29)
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Potwar Plateau (14)
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Indus River (12)
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Indus-Yarlung Zangbo suture zone (14)
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Karakoram (31)
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Geological and geotechnical evaluation of the tunnel site of the Koto Hydropower Project, Khyber Pakhtunkhwa, Pakistan
Amphibole fractionation and its potential redox effect on arc crust: Evidence from the Kohistan arc cumulates
Synthetic modeling and field GPR survey to understand the near-surface deformation induced by coseismic groundwater dynamics following the 2019 Mirpur earthquake in Pakistan
Mafic magma-driven magmatic processes and compositional variation in granitic pluton construction: The Buya intrusion of West Kunlun, Northwestern China
2019 M w 5.9 Mirpur, Pakistan Earthquake: Insights from Integrating Geodetic, Seismic, and Field Observations
Source Parameters and Slip Distribution of the 2019 M w 5.8 Mirpur (Pakistan) Earthquake Inferred from the Corrected InSAR Observations
Electron Backscatter Diffraction Study of Ultrahigh-Pressure Tso Morari Eclogites (Trans-Himalayan Collisional Zone): Implications for Strain Regime Transition from Constrictional to Plane Strain during Exhumation
RECOGNITION OF A 600-KM-LONG LATE TRIASSIC RARE METAL (Li-Rb-Be-Nb-Ta) PEGMATITE BELT IN THE WESTERN KUNLUN OROGENIC BELT, WESTERN CHINA
First report of Acanthochaetetes (Porifera: Demospongiae) from the Cretaceous Khalsi Formation, Ladakh Himalaya, India
Jurassic–Cretaceous arc magmatism along the Shyok–Bangong Suture of NW Himalaya: formation of the peri-Gondwana basement to the Ladakh Arc
Modern pollen and non-pollen palynomorphs along an altitudinal transect in Jammu and Kashmir (Western Himalaya), India
ABSTRACT The southeast Ladakh (India) area displays one of the best-preserved ophiolite sections in this planet, in places up to 10 km thick, along the southern bank of the Indus River. Recently, in situ, ultrahigh-pressure (UHP) mineralogical evidence from the mantle transition zone (MTZ; ~410–660 km) with diamond and reduced fluids were discovered from two peridotite bodies in the basal mantle part of this Indus ophiolite. Ultrahigh-pressure phases were also found by early workers from podiform chromitites of another coeval Neo-Tethyan ophiolite in southern Tibet. However, the MTZ phases in the Indus ophiolite are found in silicate peridotites, but not in metallic chromitites, and the peridotitic UHP phases show systematic and contiguous phase transitions from the MTZ to shallower depth, unlike the discrete UHP inclusions, all in Tibetan chromitites. We observe consistent change in oxygen fugacity ( f O 2 ) and fluid composition from (C-H + H 2 ) to (CO 2 + H 2 O) in the upwelling peridotitic mantle, causing melting to produce mid-ocean-ridge basalt (MORB). At shallow depths (<100 km) the free water stabilizes into hydrous phases, such as pargasitic amphibole, capable of storing water and preventing melting. Our discoveries provide unique insights into deep sub-oceanic-mantle processes, and link deep-mantle upwelling and MORB genesis. Moreover, the tectonic setting of Neo-Tethyan ophiolites has been a difficult problem since the birth of the plate-tectonics concept. This problem for the origin of ophiolites in mid-ocean-ridge versus supra-subduction zone settings clearly confused the findings from Indus ophiolites. However, in this contribution, we provide arguments in favor of mid-ocean-ridge origin for Indus ophiolite. In addition, we venture to revisit the “historical contingency” model of E.M. Moores and others for Neo-Tethyan ophiolite genesis based on the available evidence and have found that our new results strongly support the “historical contingency” model.
The dynamic response of coseismic liquefaction-induced ruptures associated with the 2019 M w 5.8 Mirpur, Pakistan, earthquake using HVSR measurements
Multi-stage India-Asia collision: Paleomagnetic constraints from Hazara-Kashmir syntaxis in the western Himalaya
(U-Th)/He Thermochronology of the Indus Group, Ladakh, Northwest India: Is Neogene Cooling a Continental-Scale Thermal Event in the India-Asia Collision Zone?
Late Pleistocene–Holocene flood history, flood-sediment provenance and human imprints from the upper Indus River catchment, Ladakh Himalaya
How Himalayan collision stems from subduction
ABSTRACT We defined the timing of surface abandonment for 10 alluvial and debris-flow fans across contrasting climatic settings in the NW Himalaya of northern India using cosmogenic 10 Be surface exposure dating. Debris-flow fans in the Garhwal, Kullu, and Lahul-Spiti regions of the monsoon-influenced Greater Himalaya were largely abandoned during the Mid- to Late Holocene. Large alluvial fans and smaller debris-flow fans in the semiarid Ladakh region of the Greater and Tethyan Himalaya have surface ages that extend throughout the last glacial. Regional events of landform abandonment and incision were defined for the monsoon-influenced western Himalaya ranges and the semiarid western Himalaya ranges over the past ~120 k.y. In the monsoon-influenced and semiarid western Himalaya ranges, these regional events were limited to the Holocene and from ca. 40 ka, respectively. The timing of fan surface abandonment and regional landform abandonment events coincided with periods of weakening monsoon strength and cooling, and local and regional glacier advances. Regional incision events from the monsoon-influenced and semiarid western Himalaya regions were recognized across various climatic conditions due to the ubiquitous nature of erosion in mountain settings. This study showed that climate-driven processes and glaciation were important drivers in fan sedimentation, catchment sediment flux, and the topographic evolution of the NW Himalaya during the late Quaternary.