current marks
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Author(s):  
Darwance Darwance ◽  
Sudarto Sudarto

The development of brand functions which was originally only as a distinguishing element to be more of a reputation, to be the brand that is usually represented by the image, logos, etc., resulting in a brand being one of the triggers for a dispute. Therefore, a number of regulations that provide protection for marks have been issued in Indonesia started with the Trademark Law of 1885 published by the Dutch Colonial Government until Law Number 20 of 2016 concerning Current Marks and Geographical Indications. But, trademark disputes still occur. This juridical normative research with a legal approach aims to know and analyze the legal politics of trademark registration regulations in Indonesia. The result is that there are weaknesses in the existing regulations regarding trademark registration, both substantial and procedural. Therefore, they need to be clearer and more concrete regulations in regulating trademark registration in Indonesia so that trademark disputes can be minimized.


2019 ◽  
Vol 0 (1) ◽  
pp. 62-66
Author(s):  
Viktor Teodosovych Bachynskyi ◽  
Oleh Yaroslavovych Vanchuliak ◽  
Ivan Hryhorovych Savka ◽  
Marta Slavivna Garazdiuk ◽  
Serhii Volodymyrovych Kozlov ◽  
...  

2013 ◽  
Vol 15 (5) ◽  
pp. 283-287 ◽  
Author(s):  
Naoko Tanaka ◽  
Hiroshi Kinoshita ◽  
Mostofa Jamal ◽  
Mitsuru Kumihashi ◽  
Kunihiko Tsutsui ◽  
...  

2003 ◽  
Vol 48 (3) ◽  
pp. 2002008 ◽  
Author(s):  
S. Anders ◽  
M. Junge ◽  
F. Schulz ◽  
K. Püschel
Keyword(s):  
Stun Gun ◽  

1959 ◽  
Vol S7-I (6) ◽  
pp. 578-582 ◽  
Author(s):  
Jean Aubouin

Abstract Describes graded bedding and current marks in microbrecciated limestones that are free of any terrigenous material. These microbreccias have been deposited on the flanks of geosynclines. It is thus shown that the existence of turbidity currents is independent of the nature of the material transported, as should be expected. From a stratigraphic point of view, the interpretation of these microbreccias requires great caution. They are monogenic, rather than polygenic. Examples are cited from the Senonian (Cretaceous) limestones of the Ionian trough (Greece).


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