Cenozoic tectonic evolution of the Himalayan orogen as constrained by along-strike variation of structural geometry, exhumation history, and foreland sedimentation
A Yin - Earth-Science Reviews, 2006 - Elsevier
Despite a long research history over the past 150 years, the geometry, kinematics, and
dynamic evolution of the Himalayan orogen remain poorly understood. This is mainly due to …
dynamic evolution of the Himalayan orogen remain poorly understood. This is mainly due to …
20 years of geological mapping of the metamorphic core across Central and Eastern Himalayas
The largest crystalline unit representing the mid-crust in the Himalayan belt is the Greater
Himalayan Sequence (GHS) which stretches all over the 2400 km of length of the belt. The …
Himalayan Sequence (GHS) which stretches all over the 2400 km of length of the belt. The …
Channel flow, ductile extrusion and exhumation in continental collision zones: an introduction
The channel flow model aims to explain features common to metamorphic hinterlands of
some collisional orogens, notably along the Himalaya-Tibet system. Channel flow describes …
some collisional orogens, notably along the Himalaya-Tibet system. Channel flow describes …
The structural geometry, metamorphic and magmatic evolution of the Everest massif, High Himalaya of Nepal–South Tibet
This paper presents a new geological map together with cross-sections and lateral sections
of the Everest massif. We combine field relations, structural geology, petrology …
of the Everest massif. We combine field relations, structural geology, petrology …
Two-mica and tourmaline leucogranites from the Everest–Makalu region (Nepal–Tibet). Himalayan leucogranite genesis by isobaric heating?
D Visonà, B Lombardo - Lithos, 2002 - Elsevier
In the Higher Himalaya of the region from Cho Oyu to the Arun valley northeast of Makalu,
the Miocene leucogranites are not hosted only in the upper High Himalayan Crystallines …
the Miocene leucogranites are not hosted only in the upper High Himalayan Crystallines …
Records of the evolution of the Himalayan orogen from in situ Th–Pb ion microprobe dating of monazite: Eastern Nepal and western Garhwal
In situ Th–Pb monazite ages from rocks collected along two transects (the Dudh Kosi-
Everest, eastern Nepal and the Bhagirathi River, Garhwal Himalaya, India) perpendicular to …
Everest, eastern Nepal and the Bhagirathi River, Garhwal Himalaya, India) perpendicular to …
Timing of midcrustal metamorphism, melting, and deformation in the Mount Everest region of southern Tibet revealed by U (-Th)-Pb geochronology
Abstract U (-Th)-Pb dating of zircon, monazite, and xenotime from metamorphic and igneous
rocks at two outcrops along a north-south transect in the Mount Everest region of southern …
rocks at two outcrops along a north-south transect in the Mount Everest region of southern …
[PDF][PDF] 印度-亚洲碰撞: 从挤压到走滑的构造转换
许志琴， 王勤， 李忠海， 李化启， 蔡志慧， 梁凤华… - 地质学报, 2016 - researchgate.net
内容提要印度= 亚洲板块碰撞导致喜马拉雅山脉的崛起% 青藏高原的生长%
两倍于正常地壳厚度的巨厚陆壳体# 以及大量青藏高原腹地的物质沿着大型走滑断裂朝东 …
两倍于正常地壳厚度的巨厚陆壳体# 以及大量青藏高原腹地的物质沿着大型走滑断裂朝东 …
Late Oligocene high‐temperature shear zones in the core of the Higher Himalayan Crystallines (Lower Dolpo, western Nepal)
A high‐temperature shear zone, Toijem shear zone, with a top‐to‐the‐SW sense of shear
affects the core of the Higher Himalayan Crystallines (HHC) in western Nepal. The shear …
affects the core of the Higher Himalayan Crystallines (HHC) in western Nepal. The shear …
Geochronology of granulitized eclogite from the Ama Drime Massif: Implications for the tectonic evolution of the South Tibetan Himalaya
The Ama Drime Massif (ADM) is an elongate north‐south trending antiformal feature that
extends∼ 70 km north across the crest of the South Tibetan Himalaya and offsets the …
extends∼ 70 km north across the crest of the South Tibetan Himalaya and offsets the …