Structural architecture and tectonic evolution of the Fangzheng sedimentary basin (NE China), and implications for the kinematics of the Tan-Lu fault zone

D. Chen; Fengqi Zhang; H. Chen; Y. Dilek; S. Yang; Q. Meng; C. Yang

doi:10.1016/j.jseaes.2015.02.028

Structural architecture and tectonic evolution of the Fangzheng sedimentary basin (NE China), and implications for the kinematics of the Tan-Lu fault zone

D. Chen
, Fengqi Zhang
, H. Chen
, Y. Dilek
, S. Yang
, Q. Meng
, C. Yang

Research output: Contribution to journal › Article › peer-review

28 Citations (Scopus)

Abstract

© 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

Original language	English
Pages (from-to)	34-48
Journal	Journal of Asian Earth Sciences
Volume	106
DOIs	https://doi.org/10.1016/j.jseaes.2015.02.028
Publication status	Published - 2015

Access to Document

10.1016/j.jseaes.2015.02.028

Cite this

@article{ac64872444524d198cf8d570f6f6b8cc,

title = "Structural architecture and tectonic evolution of the Fangzheng sedimentary basin (NE China), and implications for the kinematics of the Tan-Lu fault zone",

abstract = "{\textcopyright} 2015 Elsevier Ltd. The \textasciitilde{}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",

author = "D. Chen and Fengqi Zhang and H. Chen and Y. Dilek and S. Yang and Q. Meng and C. Yang",

year = "2015",

doi = "10.1016/j.jseaes.2015.02.028",

language = "English",

volume = "106",

pages = "34--48",

journal = "Journal of Asian Earth Sciences",

issn = "1367-9120",

publisher = "Elsevier",

}

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 -

Structural architecture and tectonic evolution of the Fangzheng sedimentary basin (NE China), and implications for the kinematics of the Tan-Lu fault zone

Abstract

Access to Document

Fingerprint

Cite this