International audienceThe Lo River fault near Tam Dao, North Vietnam, is a young, right-lateral, normal fault which has been active throughout the Quaternary. Rates of dextral slip range between 1 and 2 mm/yr whereas rates of uplift can be estimated roughly at 0.1?1 mm/yr. The drainage deflection and arrangement of shutter ridges suggest 1.5?2.0 km of dextral offset during the past 1?2 millions of years (m. y.), and the height of the youngest faceted spurs averages at 170 m. Analysis of morphometric parametres of the mountain front at Tam Dao indicates that this segment shows properties typical for nearly rectilinear, young normal scarps that belong to class I or II of relative tectonic activity and that are capable of generating strong ear...
[[abstract]]ABSTRACT In order to study the strain evolution of the highly deformed Red River Shear Z...
The northeastward motion of the Tibetan Plateau along the Altyn Tagh strike‐slip fault causes thrust...
Slip rates across active faults and folds show that late Quaternary faulting is distributed across t...
The Lo River fault near Tam Dao, North Vietnam, is a young, right-lateral, normal fault which has ...
The 900-km-long right-slip Red River fault of southernmost China and northern Vietnam is a profound ...
In SE Asia, the ca. 350 km long and up to 20 km wide Red River Shear Zone (RSZ) in NW Vietnam is com...
The 900-km-long right-slip Red River fault of southernmost China and northern Vietnam is a profound ...
The Red River fault is an important plate‐boundary fault that has played a significant role in the t...
International audienceUsing multispectral SPOT images and 1/100,000 topographic data, we present an ...
The Day Nui Con Voi massif bears a record of the Red River shear zone (RRSZ) activity in North Vietn...
International audienceFollowing the India-Asia collision, continental blocks were extruded along lar...
A new set of zircon and apatite fission-track ages from the Ailao Shan and Day Nui Con Voi (DNCV) me...
The Nam Con Son Basin is one of several Tertiary rift basins located on the continental shelf, offsh...
How the Tibetan Plateau was constructed and evolved in response to ongoing India-Asia convergence si...
Strefa uskoku Rzeki Czerwonej wyznacza granicę pomiędzy blokami Chin południowych i Indochinami. Był...
[[abstract]]ABSTRACT In order to study the strain evolution of the highly deformed Red River Shear Z...
The northeastward motion of the Tibetan Plateau along the Altyn Tagh strike‐slip fault causes thrust...
Slip rates across active faults and folds show that late Quaternary faulting is distributed across t...
The Lo River fault near Tam Dao, North Vietnam, is a young, right-lateral, normal fault which has ...
The 900-km-long right-slip Red River fault of southernmost China and northern Vietnam is a profound ...
In SE Asia, the ca. 350 km long and up to 20 km wide Red River Shear Zone (RSZ) in NW Vietnam is com...
The 900-km-long right-slip Red River fault of southernmost China and northern Vietnam is a profound ...
The Red River fault is an important plate‐boundary fault that has played a significant role in the t...
International audienceUsing multispectral SPOT images and 1/100,000 topographic data, we present an ...
The Day Nui Con Voi massif bears a record of the Red River shear zone (RRSZ) activity in North Vietn...
International audienceFollowing the India-Asia collision, continental blocks were extruded along lar...
A new set of zircon and apatite fission-track ages from the Ailao Shan and Day Nui Con Voi (DNCV) me...
The Nam Con Son Basin is one of several Tertiary rift basins located on the continental shelf, offsh...
How the Tibetan Plateau was constructed and evolved in response to ongoing India-Asia convergence si...
Strefa uskoku Rzeki Czerwonej wyznacza granicę pomiędzy blokami Chin południowych i Indochinami. Był...
[[abstract]]ABSTRACT In order to study the strain evolution of the highly deformed Red River Shear Z...
The northeastward motion of the Tibetan Plateau along the Altyn Tagh strike‐slip fault causes thrust...
Slip rates across active faults and folds show that late Quaternary faulting is distributed across t...