研究进展

钟亚婷,Kusky Timothy,王璐,GEOLOGY,2022

发表时间:2022-06-22编辑:余淳梅点击:

Giant sheath-folded nappe stack demonstrates extreme subhorizontal shear strain in an Archean orogen

作者:

Zhong, YT (Zhong, Yating) [1] , [2] ;     Kusky, TM (Kusky, Timothy M.) [1] , [2] , [3] ;     Wang, L (Wang, Lu) [1] , [2]  

GEOLOGY

50  

5  

577-582  

DOI

10.1130/G49599.1

出版时间

MAY 1 2022

已索引

2022-05-16

文献类型

Article

摘要

Giant sheath-folded nappes are associated with suture zones and emplacement of far-traveled allochthons in Phanerozoic orogens, demonstrating a rare but significant geologic phenomenon indicative of modern-style plate tectonics. We document the world's oldest-known subhorizontal mega-scale sheath fold from Archean Alpine-style nappes of the Central orogenic belt, North China craton. The Zanhuang nappes are recumbent Alpine-style forearcaffinity metabasaltic and metasedimentary nappes emplaced over a passive continental margin in the Archean, marking an ancient suture zone. Field evidence shows multiscale sheath folds from decimeters to tens of meters in size, and our three-dimensional fence profile, fold hinges, kinematic lineations, and lithological traces define an similar to 1-km-long (parallel to the x-axis) sheath fold in the core of the nappe stack. Structural analysis statistically demonstrates the macro-scale recumbent sheath-folded nappe preserves a complete 180 degrees hinge-line curvature. The giant sheath fold plunges northwest, reflecting its formation during non-coaxial, top-to-the-southeast shearing with extremely high shear strain (gamma >= 10), equated to >10 km of ductile slip on the bounding surfaces. Slip vectors derived from S-C fabrics on overturned limbs are consistent with rotation into the southeast-directed transport direction, parallel to the similarly rotated fold hinges. Comparison of the giant sheath-folded nappes from the Archean Zanhuang example with mega-scale sheath folds in Phanerozoic and Proterozoic orogens shows that Neoarchean lithosphere was stiff enough to allow tectonics to operate in a manner analogous to modern-style plate tectonics.

关键词


作者信息

通讯作者地址

Kusky, Timothy M.    

(通讯作者)

      China Univ Geosci, SchEarthSci, State Key Lab Geol Proc & Mineral Resources,Wuhan430074, Peoples R China      

所属机构

China University of Geosciences

通讯作者地址

Kusky, Timothy M.    

(通讯作者)

      China Univ Geosci, Ctr Global Tecton, SchEarthSci,Wuhan430074, Peoples R China      

所属机构

China University of Geosciences

通讯作者地址

Kusky, Timothy M.    

(通讯作者)

      China Univ Geosci, Badong Natl Observat & Res Stn Geohazards,Wuhan430074, Peoples R China      

所属机构

China University of Geosciences

地址

         
      2 China Univ Geosci, Ctr Global Tecton, SchEarthSci,Wuhan430074, Peoples R China      

所属机构

China University of Geosciences
     
      3 China Univ Geosci, Badong Natl Observat & Res Stn Geohazards,Wuhan430074, Peoples R China      

所属机构

China University of Geosciences
 


电子邮件地址

tkusky@gmail.com  

类别/分类

研究方向

Geology