The early Paleozoic cumulate gabbroic rocks from the southwest part of the Tisza Mega-Unit (Mt. Papuk, NE Croatia): evidence of a Gondwana suture zone

2020 ◽  
Vol 109 (6) ◽  
pp. 2209-2233
Author(s):  
Damir Slovenec ◽  
Mirko Belak ◽  
Ivan Mišur ◽  
Branimir Šegvić ◽  
Ralf Schuster
2019 ◽  
Vol 55 (6) ◽  
pp. 4733-4747
Author(s):  
Sainan Wu ◽  
Jiang‐Feng Qin ◽  
Shao‐Cong Lai ◽  
Xiao‐Ping Long ◽  
Yin‐Juan Ju ◽  
...  

2012 ◽  
Vol 58 (8) ◽  
pp. 920-930 ◽  
Author(s):  
BaoDi Wang ◽  
LiQuan Wang ◽  
GuiTang Pan ◽  
FuGuang Yin ◽  
DongBing Wang ◽  
...  

2019 ◽  
Vol 70 ◽  
pp. 151-170 ◽  
Author(s):  
Quyen Minh Nguyen ◽  
Qinglai Feng ◽  
Jian-Wei Zi ◽  
Tianyu Zhao ◽  
Hai Thanh Tran ◽  
...  

Author(s):  
Eugene J. Amaral

Examination of sand grain surfaces from early Paleozoic sandstones by electron microscopy reveals a variety of secondary effects caused by rock-forming processes after final deposition of the sand. Detailed studies were conducted on both coarse (≥0.71mm) and fine (=0.25mm) fractions of St. Peter Sandstone, a widespread sand deposit underlying much of the U.S. Central Interior and used in the glass industry because of its remarkably high silica purity.The very friable sandstone was disaggregated and sieved to obtain the two size fractions, and then cleaned by boiling in HCl to remove any iron impurities and rinsed in distilled water. The sand grains were then partially embedded by sprinkling them onto a glass slide coated with a thin tacky layer of latex. Direct platinum shadowed carbon replicas were made of the exposed sand grain surfaces, and were separated by dissolution of the silica in HF acid.


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