Published March 2019 | Version v1
Journal article

An efficient scheme for multi-GPU TTI reverse time migration

  • 1. China University of Geosciences-Beijing (China)
  • 2. Sinopec Geophysical Research Institute (China)

Description

Reverse time migration (RTM) is an indispensable but computationally intensive seismic exploration technique. Graphics processing units (GPUs) by NVIDIA® offer the option for parallel computations and speed improvements in such high-density processes. With increasing seismic imaging space, the problems associated with multi-GPU techniques need to be addressed. We propose an efficient scheme for multi-GPU programming based on the features of the compute-unified device Architecture (CUDA) using GPU hardware, including concurrent kernel execution, CUDA streams, and peer-to-peer (P2P) communication between the different GPUs. In addition, by adjusting the computing time for imaging during RTM, the data communication times between GPUs become negligible. This means that the overall computation efficiency improves linearly, as the number of GPUs increases. We introduce the multi-GPU scheme by using the acoustic wave propagation and then describe the implementation of RTM in tilted transversely isotropic (TTI) media. Next, we compare the multi-GPU and the unified memory schemes. The results suggest that the proposed multi-GPU scheme is superior and, with increasing number of GPUs, the computational efficiency improves linearly.

Additional details

Identifiers

Publishing Information

Journal Title
Applied Geophysics (Online)
Journal Volume
16
Journal Issue
1
Journal Page Range
p. 56-63
ISSN
1993-0658

INIS

Country of Publication
China
Country of Input or Organization
International Atomic Energy Agency (IAEA)
INIS RN
54084615
Subject category
S58: GEOSCIENCES;
Descriptors DEI
ACOUSTICS; CALCULATION METHODS; COMPUTERIZED SIMULATION; DENSITY; PROGRAMMING; SOUND WAVES; WAVE PROPAGATION
Descriptors DEC
PHYSICAL PROPERTIES; SIMULATION

Optional Information

Copyright
Copyright (c) 2018 The Editorial Department of APPLIED GEOPHYSICS. All rights reserved