Deepwater fold and thrust belt classification, tectonics, structure and hydrocarbon prospectivity: A review
Deepwater fold and thrust belts (DWFTBs) are classified into near-field stress-driven Type 1
systems confined to the sedimentary section, and Type 2 systems deformed by either far …
systems confined to the sedimentary section, and Type 2 systems deformed by either far …
The tectonic and metallogenic framework of Myanmar: A Tethyan mineral system
Myanmar is perhaps one of the world's most prospective but least explored minerals
jurisdictions, containing important known deposits of tin, tungsten, copper, gold, zinc, lead …
jurisdictions, containing important known deposits of tin, tungsten, copper, gold, zinc, lead …
Locked and loading megathrust linked to active subduction beneath the Indo-Burman Ranges
Abstract The Indo-Burman mountain ranges mark the boundary between the Indian and
Eurasian plates, north of the Sumatra–Andaman subduction zone. Whether subduction still …
Eurasian plates, north of the Sumatra–Andaman subduction zone. Whether subduction still …
Neo-Tethyan magmatism and metallogeny in Myanmar–An Andean analogue?
Plate margin tectonism, magmatic and hydrothermal processes, and the genesis of mineral
deposits are intricately linked. In Myanmar two near-parallel magmatic belts, that together …
deposits are intricately linked. In Myanmar two near-parallel magmatic belts, that together …
Weak crust in southeast Tibetan plateau revealed by Lg‐wave attenuation tomography: Implications for crustal material escape
The continuous convergence between the Indian and Eurasian plates caused massive
lithospheric deformation in the Tibetan Plateau and led to excessive crustal material …
lithospheric deformation in the Tibetan Plateau and led to excessive crustal material …
The crustal architecture of Myanmar imaged through zircon U-Pb, Lu-Hf and O isotopes: Tectonic and metallogenic implications
The Tethys margin in central and eastern Asia is comprised of continental terranes
separated by suture zones, some of which remain cryptic. Determining the crustal …
separated by suture zones, some of which remain cryptic. Determining the crustal …
Direct structural evidence of Indian continental subduction beneath Myanmar
Indian continental subduction can explain Cenozoic crustal deformation, magmatic activity
and uplift of the Tibetan Plateau following the India-Asia collision. In the western Himalayan …
and uplift of the Tibetan Plateau following the India-Asia collision. In the western Himalayan …
Structural and tectonic development of the Indo-Burma ranges
Abstract The Indo-Burma Ranges form an enigmatic mountain belt, with fragments of
evidence for an early accretionary history (Jurassic Jade belt HP-LT metamorphism; Early …
evidence for an early accretionary history (Jurassic Jade belt HP-LT metamorphism; Early …
Tectonic and metamorphic evolution of the Mogok Metamorphic and Jade Mines belts and ophiolitic terranes of Burma (Myanmar)
The Mogok Metamorphic Belt is a north–south-aligned belt of mainly high-grade
metamorphic rocks and granites that extends the length of Burma (Myanmar) along the …
metamorphic rocks and granites that extends the length of Burma (Myanmar) along the …
New GNSS and geological data from the Indo‐Burman subduction zone indicate active convergence on both a locked megathrust and the Kabaw Fault
Abstract The Indo‐Burma subduction zone is a highly oblique subduction system where the
Indian plate is converging with the Eurasian plate. How strain is partitioned between the …
Indian plate is converging with the Eurasian plate. How strain is partitioned between the …