TY - GEN
T1 - 3D structural geological modeling based on morphing field
AU - Xianhai, Meng
AU - Jigang, Li
AU - Qin, Yang
PY - 2012
Y1 - 2012
N2 - Strata are continuous surface by sediment, which form fractured and discontinuous geological layers during strata moving. In 3D structural geological modeling, how to describe fractured geological layers well and truly is a complicated problem. Now most software such as RCRC's 3D Earth Modeling, Petrel's advanced 3D Reservoir Modeling, ROXAR's RMS, T-Surf's GOCAD, create strata by user interactive editing during 3D geological modeling. Only little commercial software such as DGI's Earth Vision Modeling System realizes the function of creating discontinuous strata by strata point set and faults directly. At present, we can't yet search correlative algorithm in open literature.
AB - Strata are continuous surface by sediment, which form fractured and discontinuous geological layers during strata moving. In 3D structural geological modeling, how to describe fractured geological layers well and truly is a complicated problem. Now most software such as RCRC's 3D Earth Modeling, Petrel's advanced 3D Reservoir Modeling, ROXAR's RMS, T-Surf's GOCAD, create strata by user interactive editing during 3D geological modeling. Only little commercial software such as DGI's Earth Vision Modeling System realizes the function of creating discontinuous strata by strata point set and faults directly. At present, we can't yet search correlative algorithm in open literature.
UR - https://www.scopus.com/pages/publications/82055166230
U2 - 10.1007/978-1-4471-2386-6_20
DO - 10.1007/978-1-4471-2386-6_20
M3 - 会议稿件
AN - SCOPUS:82055166230
SN - 9781447123859
T3 - Lecture Notes in Electrical Engineering
SP - 149
EP - 157
BT - Information Engineering and Applications - International Conference on Information Engineering and Applications, IEA 2011
T2 - International Conference on Information Engineering and Applications, IEA 2011
Y2 - 21 October 2011 through 23 October 2011
ER -