Southeast Asia is located in an important regional geodynamic intersection zone
surrounded by inward subduction systems on three sides, consisting the largest and most …

Abstract The Central Andaman Basin (CAB) is generally accepted to be a site of continuous
sea floor spreading since the Early Pliocene (∼ 4.0 Ma). The adjacent Alcock and Sewell …

To clarify the tectonic evolution of M15 block in the Andaman Sea, we perform a delicate
study of fault geometry and dynamics using a 3D seismic data. The data reveal eight …

Burma (Myanmar) is situated along the obliquely colliding eastern margin of the Indian Plate
(Fig. 2.1). It connects the ongoing India-Asia collision along the Himalayan Range in the …

针对我国在西南构造活跃区修建的水库蓄水与地震活动的关系, 本文对蓄水已长达7
年并在高水位运维多个周期的云南小湾水库, 采用结合波形互相关技术的双差地震定位法对水库 …

In this study, we reveal the deformational structure of the crust of the northern part of the
Ryukyu Arc and Okinawa Trough using ambient noise tomography. Compared with southern …

The injection of CO2 at the Decatur carbon capture and storage site has generated
significant microseismic activity, which occurs in distinct spatial clusters up to approximately …

We determine the deep structure of the eastern Algerian basin and its southern margin in the
Annaba region (easternmost Algeria), to better constrain the plate kinematic reconstruction …

Fluid overpressure and fluid migration are known to be able to trigger or induce fault slip.
However, relatively little is known about the role of fluids on generating earthquakes in some …

The Mawchi Mine in Myanmar is a historic world-class Sn–W deposit within the tin province
of Southeast Asia, extending from Yunnan in SW China through Myanmar and Thailand, via …