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Quantifying the rise of the Himalaya orogen and implications for the south Asian monsoon

Ding Lin, Ding Lin ; Spicer, R. A ; Yang Jian, Yang Jian ; Xu Qiang, Xu Qiang ; Cai Fulong, Cai Fulong ; Li Shun, Li Shun ; Lai Qingzhou, Lai Qingzhou ; Wang Houqi, Wang Houqi ; Spicer, T. E. V ; Yue Yahui, Yue Yahui ; Shukla, A ; Srivastava, G ; Khan, M. Ali ; Bera, S ; Mehrotra, R

Geology (Boulder), 2017-03, Vol.45 (3), p.215-218 [Periódico revisado por pares]

Boulder: Geological Society of America (GSA)

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Título:
Quantifying the rise of the Himalaya orogen and implications for the south Asian monsoon
Autor: Ding Lin, Ding Lin ; Spicer, R. A ; Yang Jian, Yang Jian ; Xu Qiang, Xu Qiang ; Cai Fulong, Cai Fulong ; Li Shun, Li Shun ; Lai Qingzhou, Lai Qingzhou ; Wang Houqi, Wang Houqi ; Spicer, T. E. V ; Yue Yahui, Yue Yahui ; Shukla, A ; Srivastava, G ; Khan, M. Ali ; Bera, S ; Mehrotra, R
Assuntos: absolute age ; Asia ; atmospheric circulation ; atmospheric precipitation ; Cenozoic ; China ; chronostratigraphy ; Deformation ; elevation ; Far East ; Fossils ; Geological time ; Himalayan Orogeny ; Himalayas ; Liuqu Conglomerate ; lower Miocene ; Miocene ; monsoons ; Mountains ; Neogene ; nesosilicates ; orogenic belts ; orogeny ; orthosilicates ; paleoaltimetry ; Paleocene ; paleoclimatology ; paleoecology ; Paleogene ; paleogeography ; paleorelief ; Plantae ; Precipitation ; quantitative analysis ; reconstruction ; sedimentary rocks ; silicates ; Stratigraphy ; Structural geology ; tectonics ; Tertiary ; U/Pb ; uplifts ; Wind ; Xizang China ; zircon ; zircon group
É parte de: Geology (Boulder), 2017-03, Vol.45 (3), p.215-218
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SourceType-Scholarly Journals-1
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Descrição: We reconstruct the rise of a segment of the southern flank of the Himalaya-Tibet orogen, to the south of the Lhasa terrane, using a paleoaltimeter based on paleoenthalpy encoded in fossil leaves from two new assemblages in southern Tibet (Liuqu and Qiabulin) and four previously known floras from the Himalaya foreland basin. U-Pb dating of zircons constrains the Liuqu flora to the latest Paleocene (ca. 56 Ma) and the Qiabulin flora to the earliest Miocene (21-19 Ma). The proto-Himalaya grew slowly against a high (∼4 km) proto-Tibetan Plateau from ∼1 km in the late Paleocene to ∼2.3 km at the beginning of the Miocene, and achieved at least ∼5.5 km by ca. 15 Ma. Contrasting precipitation patterns between the Himalaya-Tibet edifice and the Himalaya foreland basin for the past ∼56 m.y. show progressive drying across southern Tibet, seemingly linked to the uplift of the Himalaya orogen.
Editor: Boulder: Geological Society of America (GSA)
Idioma: Inglês

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Quantifying the rise of the Himalaya orogen and implications for the south Asian monsoon

Ding Lin, Ding Lin ; Spicer, R. A ; Yang Jian, Yang Jian ; Xu Qiang, Xu Qiang ; Cai Fulong, Cai Fulong ; Li Shun, Li Shun ; Lai Qingzhou, Lai Qingzhou ; Wang Houqi, Wang Houqi ; Spicer, T. E. V ; Yue Yahui, Yue Yahui ; Shukla, A ; Srivastava, G ; Khan, M. Ali ; Bera, S ; Mehrotra, R

Boulder: Geological Society of America (GSA)

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