Add to ORKGThe collision of India into Asia has produced the highest mountain belt on the planet, the Himalayas, which is often held to be the classic example of mountain building. Despite this, much about the mountain belt is not understood, including the unexpectedly vital role it plays in shaping our climate. Rowan Vernon explains more
Cenozoic convergence between the Indian and Asian plates produced the archetypical continental colli...
Over the past few decades understanding of orogen development has evolved at a rapid pace, with cla...
Prevailing dogma asserts that the uplift of Tibet, the onset of the Asian monsoon system and high bi...
Understanding the crustal evolution of any orogen is essential in delineating the nomenclature of li...
abstract: The Himalaya are the archetypal example of a continental collision belt, formed by the ong...
Convective removal of lower lithosphere beneath the Tibetan Plateau can account for a rapid increase...
AGU Fall Meeting 2013, 09.12 - 13.12.2013 , San Francisco, USAThe Himalaya-Tibet and Zagros orogens ...
abstract: The collision of India and Eurasia constructed the Himalayan Mountains. Questions remain r...
The Indo-Asian orogen is the world’s largest region of high topography, which affects both regional ...
Cenozoic convergence between the Indian and Asian plates produced the archetypical continental colli...
Many ideas about the tectonic history of the Himalayan orogen hinge on the arguments about the timin...
Tectonic models for the Oligocene–Miocene development of the Himalaya mountain range are largely foc...
Despite being the largest active collisional orogen on Earth, the growth mechanism of the Himalaya r...
The Shillong Plateau (northeastern India) constitutes the only significant topography in the Himalay...
<p>This paper presents a new geological map together with cross-sections and lateral sections of the...
Cenozoic convergence between the Indian and Asian plates produced the archetypical continental colli...
Over the past few decades understanding of orogen development has evolved at a rapid pace, with cla...
Prevailing dogma asserts that the uplift of Tibet, the onset of the Asian monsoon system and high bi...
Understanding the crustal evolution of any orogen is essential in delineating the nomenclature of li...
abstract: The Himalaya are the archetypal example of a continental collision belt, formed by the ong...
Convective removal of lower lithosphere beneath the Tibetan Plateau can account for a rapid increase...
AGU Fall Meeting 2013, 09.12 - 13.12.2013 , San Francisco, USAThe Himalaya-Tibet and Zagros orogens ...
abstract: The collision of India and Eurasia constructed the Himalayan Mountains. Questions remain r...
The Indo-Asian orogen is the world’s largest region of high topography, which affects both regional ...
Cenozoic convergence between the Indian and Asian plates produced the archetypical continental colli...
Many ideas about the tectonic history of the Himalayan orogen hinge on the arguments about the timin...
Tectonic models for the Oligocene–Miocene development of the Himalaya mountain range are largely foc...
Despite being the largest active collisional orogen on Earth, the growth mechanism of the Himalaya r...
The Shillong Plateau (northeastern India) constitutes the only significant topography in the Himalay...
<p>This paper presents a new geological map together with cross-sections and lateral sections of the...
Cenozoic convergence between the Indian and Asian plates produced the archetypical continental colli...
Over the past few decades understanding of orogen development has evolved at a rapid pace, with cla...
Prevailing dogma asserts that the uplift of Tibet, the onset of the Asian monsoon system and high bi...