TY - JOUR
T1 - Structural architecture and tectonic evolution of the Fangzheng sedimentary basin (NE China), and implications for the kinematics of the Tan-Lu fault zone
AU - Chen, D.
AU - Zhang, Fengqi
AU - Chen, H.
AU - Dilek, Y.
AU - Yang, S.
AU - Meng, Q.
AU - Yang, C.
PY - 2015
Y1 - 2015
N2 - © 2015 Elsevier Ltd. The ~100-km-long, NE-SW-trending Fangzheng sedimentary basin is one of a series of Cenozoic petroliferous depocenters along the Tan-Lu Fault Zone (TLFZ) in NE China. It is delimited by the NW and SE Boundary Faults and dissected by the basin-parallel Central Fault, all of which are part of the dextral TLFZ displaying releasing and restraining bends along-strike. The basinal strata and its pre-Cenozoic basement show well-developed transtensional and transpressional structures in these domains. The stratigraphy in the basin consists of
AB - © 2015 Elsevier Ltd. The ~100-km-long, NE-SW-trending Fangzheng sedimentary basin is one of a series of Cenozoic petroliferous depocenters along the Tan-Lu Fault Zone (TLFZ) in NE China. It is delimited by the NW and SE Boundary Faults and dissected by the basin-parallel Central Fault, all of which are part of the dextral TLFZ displaying releasing and restraining bends along-strike. The basinal strata and its pre-Cenozoic basement show well-developed transtensional and transpressional structures in these domains. The stratigraphy in the basin consists of
U2 - 10.1016/j.jseaes.2015.02.028
DO - 10.1016/j.jseaes.2015.02.028
M3 - Article
SN - 1367-9120
VL - 106
SP - 34
EP - 48
JO - Journal of Asian Earth Sciences
JF - Journal of Asian Earth Sciences
ER -