Rendiconti Online della Societa Geologica Italiana

metrics 2024

Connecting Scholars with Pioneering Geological Research

Introduction

Rendiconti Online della Societa Geologica Italiana, published by the Società Geologica Italiana, emerges as a pivotal platform for the dissemination of cutting-edge research in the field of Geology. With an ISSN of 2035-8008, this journal has been contributing to the geological discourse since its inception in 2008, offering a repository of valuable insights up until 2024. With a current classification of Q4 within the Geology category, as reported in 2023, and ranking as 251st out of 321 in the Scopus Ranks for Earth and Planetary Sciences, the journal serves as an essential, albeit developing, resource for increased visibility in the geological sciences. Researchers, professionals, and students will find in its pages a vibrant collection of articles that reflect the latest advancements, innovative methodologies, and comprehensive studies from both established and early-career scientists. The open access model further enhances its accessibility, ensuring that scholarly contributions reach a broad audience of scholars and practitioners eager to stay at the forefront of geological research.

Metrics 2024

SCIMAGO Journal Rank0.19
Journal Impact Factor0.40
Journal Impact Factor (5 years)0.40
H-Index20
Journal IF Without Self0.40
Eigen Factor0.00
Normal Eigen Factor0.04
Influence0.10
Immediacy Index0.40
Cited Half Life7.90
Citing Half Life11.80
JCI0.12
Total Documents2645
WOS Total Citations290
SCIMAGO Total Citations1733
SCIMAGO SELF Citations251
Scopus Journal Rank0.19
Cites / Document (2 Years)0.51
Cites / Document (3 Years)0.46
Cites / Document (4 Years)0.52

Metrics History

Rank 2024

Scopus

Geology in Earth and Planetary Sciences
Rank #251/321
Percentile 21.81
Quartile Q4

IF (Web Of Science)

GEOSCIENCES, MULTIDISCIPLINARY
Rank 235/253
Percentile 7.30
Quartile Q4

JCI (Web Of Science)

GEOSCIENCES, MULTIDISCIPLINARY
Rank 237/253
Percentile 6.32
Quartile Q4

Quartile History

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