Question
Asked 23 February 2023

How to find/get Scopus ID?

I published my research paper in Journal of Intelligent & Fuzzy Systems. This journal comes under iosPress and scopus index journal.
If I search my name in the "Search for an author profile" with this - https://www.scopus.com/freelookup/form/author.uri?zone=TopNavBar&origin=NO%20ORIGIN%20DEFINED - I could not find?
Can any one help regarding this Please?
Thanks in advance,
Dr. C.Rajendra Thilahar.

All Answers (3)

You may find it by using your article. If your article is indexed, it will appear in Scopus. By clicking you name in that article, you could find out your Scopus ID.
I think your article is not indexed by Scopus and it may take time to index. So you may search later.
2 Recommendations
Misgana Duresa
Madda Walabu University
I published journal in this journal. How can I get Author id
Rob Keller
Charlemagne College, Nijmegen, The Netherlands
Dear Misgana Duresa According to https://research-hub.auckland.ac.nz/researcher-profiles-and-ids/scopus-ID "You do not have to register for this ID. It is automatically assigned when you publish two or more works in a journal indexed by Scopus."
You may checked this to go to https://www.scopus.com/sources click on search/Author search and search for your name.
Best regards.
PS. For the moment only one paper is present Scopus. Once your Frontiers paper is indexed then it will resolve itself automatically.
2 Recommendations

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Dear RG community members,
I have found this sample in our rock collection used with bachelor students enrolled in Geology studies. I do not know where this rock comes from.
I have made a thin section but I have problems in classifying it. It is represented by ~30-40% andesine, ~40-50% greenish biotite (but it is not chloritized), ~5% titanite, ~5% sparry calcite and few amounts of apatite. No quartz, no white mica, no alkali feldspar nor other minerals.
Plagioclase occurs a large anhedral crystals or as minute crystals occasionally joined in triple junctions. Biotite is commonly found around ellipsoid to circular agglomerations of plagioclase. There is little evidence of schistosity, but probably this is due to the way the rocks has been cut. The macroscopic sample has clear signs of anisotropies. It is black and shining (for the great amount of mica).
According to me it cannot be a normal diorite because of the presence of triple junctions and clear anisotropy observed in the hand sample. I believe it cannot be defined as a meta-diorite, because plagioclases are grouped in a sort of "eyes" like "augen-gneiss". These "eyes" of plagioclase are either made up of single large anhedral crystals of plagioclase or are, more commonly and larger, made up of several smaller anhedral plagioclase. These plagioclase crystals look like a conglomerate, but it is unrealistic to believe that this is a meta-conglomerate because there is no quartz, no alkali feldspars and plagioclase are completely fresh and without any kind of cement and without white mica.
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Attached some pictures of the rock taken with my smartphone (sorry for the poor quality).
Cheers,
michele

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