Structural and geochemical studies on amphibolite and greenschist-facies rocks in the Kulidjik river valley, eastern Rhodope, Bulgaria: preliminary results

2006 ◽  
Vol 239 (2) ◽  
pp. 161-181
Author(s):  
Nikolay Bonev
2022 ◽  
Vol 962 (1) ◽  
pp. 012059
Author(s):  
R V Shtokalo ◽  
N A Krivolutskaya ◽  
A A Konyshev ◽  
I T Rass ◽  
S I Demidova

Abstract We studied 6 sections of the Arydzhangsky lava formation (P2-T1) in the Kotuy river valley. The results of petrographic and geochemical studies of the composition of rocks of the Arydzhangsky, Khardaksky and Pravoboyarsky formations are presented. The stratigraphic columns of the sections were built and the composition of the rocks was additionally determined using a scanning electron microscope. In this regard, the relative position of these formations was established, the mantle and crust sources of magmas were confirmed. A geochemical identity of the rocks of the Khardaksky formation with the rocks of the Arydzhangsky formation was established, which suggests a similar age of their formation.


1998 ◽  
Vol 29 (5-7) ◽  
pp. 1779-1795 ◽  
Author(s):  
Pim F van Bergen ◽  
Chris J Nott ◽  
Ian D Bull ◽  
Paul R Poulton ◽  
Richard P Evershed

2006 ◽  
Vol 40 (34) ◽  
pp. 6650-6665 ◽  
Author(s):  
Reddy L.N. Yatavelli ◽  
Jason K. Fahrni ◽  
Myoungwoo Kim ◽  
Kevin C. Crist ◽  
Christopher D. Vickers ◽  
...  

2020 ◽  
Author(s):  
Daniel Gardner ◽  
◽  
Shanti Penprase ◽  
Phillip H. Larson ◽  
Andrew D. Wickert ◽  
...  

2021 ◽  
Vol 8 (1) ◽  
pp. 35-39
Author(s):  
Krzysztof Żurek ◽  
Tomasz Kalicki ◽  
Fularczyk Karolina ◽  
Paweł Przepióra ◽  
Piotr Kusztal

1999 ◽  
Vol 173 ◽  
pp. 185-188
Author(s):  
Gy. Szabó ◽  
K. Sárneczky ◽  
L.L. Kiss

AbstractA widely used tool in studying quasi-monoperiodic processes is the O–C diagram. This paper deals with the application of this diagram in minor planet studies. The main difference between our approach and the classical O–C diagram is that we transform the epoch (=time) dependence into the geocentric longitude domain. We outline a rotation modelling using this modified O–C and illustrate the abilities with detailed error analysis. The primary assumption, that the monotonity and the shape of this diagram is (almost) independent of the geometry of the asteroids is discussed and tested. The monotonity enables an unambiguous distinction between the prograde and retrograde rotation, thus the four-fold (or in some cases the two-fold) ambiguities can be avoided. This turned out to be the main advantage of the O–C examination. As an extension to the theoretical work, we present some preliminary results on 1727 Mette based on new CCD observations.


2000 ◽  
Vol 179 ◽  
pp. 163-165
Author(s):  
S. K. Solanki ◽  
M. Fligge ◽  
P. Pulkkinen ◽  
P. Hoyng

AbstractThe records of sunspot number, sunspot areas and sunspot locations gathered over the centuries by various observatories are reanalysed with the aim of finding as yet undiscovered connections between the different parameters of the sunspot cycle and the butterfly diagram. Preliminary results of such interrelationships are presented.


1978 ◽  
Vol 48 ◽  
pp. 31-35
Author(s):  
R. B. Hanson

Several outstanding problems affecting the existing parallaxes should be resolved to form a coherent system for the new General Catalogue proposed by van Altena, as well as to improve luminosity calibrations and other parallax applications. Lutz has reviewed several of these problems, such as: (A) systematic differences between observatories, (B) external error estimates, (C) the absolute zero point, and (D) systematic observational effects (in right ascension, declination, apparent magnitude, etc.). Here we explore the use of cluster and spectroscopic parallaxes, and the distributions of observed parallaxes, to bring new evidence to bear on these classic problems. Several preliminary results have been obtained.


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