Competency contrast, kinematics, and the development of foliations and lineations in the crust

LB Goodwin, B Tikoff - Journal of structural Geology, 2002 - Elsevier
Similar foliation patterns are observed in faults in poorly lithified sediments, fault gouge and
cataclasite, and greenschist to granulite facies shear zones. We suggest that this similarity in …
被引用次数：156 相关文章

COMPETENCY CONTRAST, KINEMATICS, AND THE DEVELOPMENT OF FOLIATIONS AND LINEATIONS IN THE CRUST

LB Goodwin, B Tikoff - 2002 - repository.geologyscience.ru
Similar foliation patterns are observed in faults in poorly lithified sediments, fault gouge and
cataclasite, and greenschist to granulite facies shear zones. We suggest that this similarity in …

[引用][C] Competency contrast, kinematics, and the development of foliations and lineations in the crust

LB Goodwin, B Tikoff - Journal of Structural Geology, 2002 - cir.nii.ac.jp
Competency contrast, kinematics, and the development of foliations and lineations in the
crust | CiNii Research CiNii 国立情報学研究所 学術情報ナビゲータ[サイニィ] 詳細へ移動 検索 …

Competency contrast, kinematics, and the development of foliations and lineations in the crust

LB Goodwin, B Tikoff - Journal of Structural Geology, 2002 - infona.pl
Similar foliation patterns are observed in faults in poorly lithified sediments, fault gouge and
cataclasite, and greenschist to granulite facies shear zones. We suggest that this similarity in …

Competency contrast, kinematics, and the development of foliations and lineations in the crust

LB Goodwin, B Tikoff - Journal of Structural Geology, 2002 - ui.adsabs.harvard.edu
Similar foliation patterns are observed in faults in poorly lithified sediments, fault gouge and
cataclasite, and greenschist to granulite facies shear zones. We suggest that this similarity in …

Competency contrast, kinematics, and the development of foliations and lineations in the crust

LB Goodwin, B Tikoff - Journal of Structural Geology, 2002 - elibrary.ru
Similar foliation patterns are observed in faults in poorly lithified sediments, fault gouge and
cataclasite, and greenschist to granulite facies shear zones. We suggest that this similarity in …