Zobrazeno 1 - 10
of 60
pro vyhledávání: '"Yani Najman"'
Autor:
Guillaume Dupont-Nivet, Niels Meijer, Lin Li, Marc Poujol, Mustafa Kaya, Jovid Aminov, Yani Najman
Publikováno v:
Basin Research
Basin Research, 2022, 34 (2), pp.533-554. ⟨10.1111/bre.12629⟩
Basin Research, Wiley, In press, ⟨10.1111/bre.12629⟩
Basin Research, 2022, 34 (2), pp.533-554. ⟨10.1111/bre.12629⟩
Basin Research, Wiley, In press, ⟨10.1111/bre.12629⟩
International audience; How and when the Pamir formed remains an open question. This study explores Pamir tectonics recorded in a sedimentary section in the eastern Tajik Basin. A prominent lithofacies change that has been recognized regionally is as
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ad29e25dd7ae6ca172b06bd84ebda4df
https://insu.hal.science/insu-03405280/document
https://insu.hal.science/insu-03405280/document
Autor:
Weiwei Xue, Yani Najman, Xiumian Hu, Cristina Persano, Finlay M. Stuart, Wei Li, Anlin Ma, Ying Wang
Publikováno v:
Tectonics. 41
Much of the interior of the Tibetan Plateau is characterized by internal drainage, low relief topography, and high altitude. How and when this landscape formed is controversial. In this study, we use new zircon U-Pb data and low-temperature thermochr
Autor:
Daniel F. Stockli, Yani Najman
Publikováno v:
Elements. 16:311-317
A dvances in detrital noble gas thermochronometry by 40Ar/39Ar and (U–Th)/He dating are improving the resolution of sedimentary provenance reconstructions and are providing new insights into the evolution of Earth’s surface. Detrital thermochrono
The Himalaya, the Earth's largest active orogen, produces a deep but relatively unexplored foreland basin by loading the Indian Plate. Newly available two-dimensional seismic data (ca. 5,180 line km) spanning 900 km of the Nepali lowlands allow mappi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::35410bceb957922b19803f5155d0499c
https://doi.org/10.1111/bre.12584
https://doi.org/10.1111/bre.12584
Autor:
Mustafa Kaya, Lin Li, Yani Najman, Pierrick Roperch, Jovid Aminov, Guillaume Dupont-Nivet, Niels Meijer
Publikováno v:
European Geosciences Union General Assembly 2021 (EGU 2021)
European Geosciences Union General Assembly 2021 (EGU 2021), Nov 2021, online, France. ⟨10.5194/egusphere-egu21-9901⟩
EGU 2021 General Assembly Conference Abstracts
European Geosciences Union General Assembly 2021 (EGU 2021), Nov 2021, online, France. ⟨10.5194/egusphere-egu21-9901⟩
EGU 2021 General Assembly Conference Abstracts
Contrasting models have been proposed to explain the formation of the Pamir salient: either largely inherited from a Mesozoic arcuate structure or recently formed by Indian northward indentation and possibly related to syn-orogenic lateral extrusion.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b1ed212dc867420b4148369ad808d95e
https://doi.org/10.5194/egusphere-egu21-9901
https://doi.org/10.5194/egusphere-egu21-9901
Autor:
Shihu Li, Yani Najman
Knowledge of the timing of India-Asia collision and associated Tethyan closure in the region is critical to advancement of models of crustal deformation. One of a number of methods traditionally used to constrain the time of India-Asia collision is t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e23d1eb9eeac451b790285298185e76a
https://doi.org/10.5194/egusphere-egu21-1916
https://doi.org/10.5194/egusphere-egu21-1916
The India‐Asia collision zone in Ladakh, northwest India, records a sequence of tectono‐thermal events in the interior of the Himalayan orogen following the intercontinental collision between India and Asia in early Cenozoic time. We present zirc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d2a285810949b631362a45e548306641
https://doi.org/10.1029/2020TC006333
https://doi.org/10.1029/2020TC006333
Publikováno v:
Proc Natl Acad Sci U S A
The Himalayan foreland basin formed by flexure of the Indian Plate below the advancing orogen. Motion on major thrusts within the orogen has resulted in damaging historical seismicity, whereas south of the Main Frontal Thrust (MFT), the foreland basi
Autor:
Yani Najman
Interrogation of sediment archives allows for documentation of both hinterland and foreland deformation. Examples of their use as an archive of Himalayan foreland deformation include the work of Govin et al. (Geology, 2018) in which determination of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fe509bca81eaea2d94eb30aca57097be
https://doi.org/10.5194/egusphere-egu2020-3800
https://doi.org/10.5194/egusphere-egu2020-3800
Knowledge of the geological history of the Tibetan plateau is critical to understanding crustal deformation process, and the plateau’s influence on climate. However, the timing of Tibetan plateau development remains controversial. The Nima Basin al
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eece39aa3c8fe5cd5d87c09d3a6e6ef1
https://doi.org/10.5194/egusphere-egu2020-5082
https://doi.org/10.5194/egusphere-egu2020-5082