The northern boundary of the Proto-Tethys Ocean: Constraints from structural analysis and U–Pb zircon geochronology of the North Qinling Terrane

2015 ◽  
Vol 113 ◽  
pp. 560-574 ◽  
Author(s):  
Shujuan Zhao ◽  
Sanzhong Li ◽  
Xin Liu ◽  
M. Santosh ◽  
I.D. Somerville ◽  
...  
2017 ◽  
Vol 52 ◽  
pp. 202-214 ◽  
Author(s):  
Shujuan Zhao ◽  
Sanzhong Li ◽  
Xiyao Li ◽  
Ian Somerville ◽  
Huahua Cao ◽  
...  

2017 ◽  
Author(s):  
Brandon Tyler Peach ◽  
◽  
David E. Blake ◽  
David E. Blake ◽  
Todd A. LaMaskin ◽  
...  

2020 ◽  
Vol 35 (S1) ◽  
pp. S38-S42
Author(s):  
Soraia Rodrigues de Azeredo ◽  
Roberto Cesareo ◽  
Angel Guillermo Bustamante Dominguez ◽  
Ricardo Tadeu Lopes

Precious ornaments from the Museum Royal Tombs of Sipán were analyzed by X-ray computed microtomography (microCT). The ornaments analyzed were golden earrings produced by the Moche culture that flourished along the north coast of present-day Peru between approximately 100 and 600 AD. Sipán, also known as Huava Rajada, is a mochica archaeological complex in the north of Peru. In particular, the spectacular jewelry, mainly composed of gold, silver, and copper alloys, gilded copper, and tumbaga, from the Museum “Royal Tombs of Sipán,” in Lambayeque, north of Peru, are some of the most sophisticated metalworking ever produced of pre-Columbian America. A portable microCT system consisting of a high-resolution flat panel detector and a mini X-ray tube were used for the structural analysis of these ornaments. The microCT images show parts of the internal structure, highlighting the manufacturing technique and gold sheets joining techniques of the Moche artisans. Furthermore, the advantage of using the portable microCT system for nondestructive testing is clear when the sample cannot be taken to the laboratory.


2014 ◽  
Vol 86 (3) ◽  
pp. 1101-1113 ◽  
Author(s):  
FABRÍCIO A. CAXITO ◽  
ALEXANDRE UHLEIN ◽  
LUIZ F.G. MORALES ◽  
MARCOS EGYDIO-SILVA ◽  
JULIO C.D. SANGLARD ◽  
...  

The Rio Preto fold belt borders the northwestern São Francisco craton and shows an exquisite kilometric doubly-vergent asymmetric fan structure, of polyphasic structural evolution attributed exclusively to the Brasiliano Orogeny (∼600-540 Ma). The fold belt can be subdivided into three structural compartments: The Northern and Southern compartments showing a general NE-SW trend, separated by the Central Compartment which shows a roughly E-W trend. The change of dip of S2, a tight crenulation foliation which is the main structure of the fold belt, between the three compartments, characterizes the fan structure. The Central Compartment is characterized by sub-vertical mylonitic quartzites, which materialize a system of low-T strike slip shear zones (Malhadinha – Rio Preto Shear Zone) crosscutting the central portion of the fold belt. In comparison to published analog models, we consider that the unique structure of the Rio Preto fold belt was generated by the oblique, dextral-sense interaction between the Cristalândia do Piauí block to the north and the São Francisco craton to the south.


2016 ◽  
Vol 61 (12) ◽  
pp. 1365-1378 ◽  
Author(s):  
ShiJie YANG ◽  
YunFei REN ◽  
Liang LIU ◽  
XiangKuan GONG ◽  
DanLing CHEN ◽  
...  

Sign in / Sign up

Export Citation Format

Share Document