Lithospheric electrical structure of the middle Lhasa terrane in the south Tibetan plateau

• Published in: Tectonophysics 2018-04, Vol.731-732, p.95-103
• Main Authors: Liang, Hongda, Jin, Sheng, Wei, Wenbo, Gao, Rui, Ye, Gaofeng, Zhang, Letian, Yin, Yaotian, Lu, Zhanwu
• Format: Article
• Language: English
• Subjects: Asthenosphere; Broadband; Collisions; Data; Data analysis; Deep processes; Earth mantle; Electrical conductivity; Electrical resistivity; Evolution; Indian-Asian collision; Inversion; Lhasa terrane; Lithosphere; Lithospheric electrical structure; Magnetic field; Magnetic fields; Magnetotelluric; Mineral deposits; Mineralization; Ocean circulation; Plates (structural members); Subduction; Transverse electric modes; Transverse magnetic modes; Two dimensional analysis; Two dimensional models; Upper mantle; Upwelling
• ISSN: 0040-1951; 1879-3266
• DOI: 10.1016/j.tecto.2018.01.020

The Lhasa terrane in southern Tibetan plateau is a huge tectono-magmatic belt and an important metallogenic belt. Its formation evolution process and mineralization are affected by the subduction of oceanic plate and subsequent continental collision. However, the evolution of Lhasa terrane has been a subject of much debate for a long time. The Lithospheric structure records the deep processes of the subduction of oceanic plate and continental collision. The magnetotelluric (MT) method can probe the sub-surface electrical conductivity, newly dense broadband and long period magnetotelluric data were collected along a south-north trending profile that across the Lhasa terrane at 88°–89°E. Dimensionality analyses demonstrated that the MT data can be interpreted using two-dimensional approaches, and the regional strike direction was determined as N110°E.Based on data analysis results, a two-dimensional (2-D) resistivity model of crust and upper mantle was derived from inversion of the transverse electric mode, transverse magnetic mode and vertical magnetic field data. Inversion model shows a large north-dipping resistor that extended from the upper crust to upper mantle beneath the Himalaya and the south of Lhasa Terrane, which may represent the subducting Indian continental lithosphere. The 31°N may be an important boundary in the Lhasa Terrane, the south performs a prominent high-conductivity anomaly from the lower crust to upper mantle which indicates the existence of asthenosphere upwelling, while the north performs a higher resistivity and may have a reworking ancient basement. The formation of the ore deposits in the study area may be related to the upwelling of the mantle material triggered by slab tearing and/or breaking off of the Indian lithosphere, and the mantle material input also contributed the total thickness of the present-day Tibetan crust. The results provide helpful constrains to understand the mechanism of the continent-continent collision and the regional exploratory prospect of the deep resources. •2D inversion for a dense MT profile in the middle Lhasa Terrane was performed.•The north of the Lhasa Terrane has different structure from the south.•The upwelling of asthenosphere may be related to slab tearing or/and breaking off of the Indian lithosphere.•The crustal thickening and the formation of ore deposits may be related to the mantle contributions.