OFIOLITI

Scope & Guideline

Elevating Geological Research to New Heights

Introduction

Welcome to the OFIOLITI information hub, where our guidelines provide a wealth of knowledge about the journal’s focus and academic contributions. This page includes an extensive look at the aims and scope of OFIOLITI, highlighting trending and emerging areas of study. We also examine declining topics to offer insight into academic interest shifts. Our curated list of highly cited topics and recent publications is part of our effort to guide scholars, using these guidelines to stay ahead in their research endeavors.
LanguageMulti-Language
ISSN0391-2612
PublisherOFIOLITI
Support Open AccessNo
CountryItaly
TypeJournal
Convergefrom 1978 to 2024
AbbreviationOFIOLITI / Ofioliti
Frequency2 issues/year
Time To First Decision-
Time To Acceptance-
Acceptance Rate-
Home Page-
AddressDIPARTIMENTO DI SCIENZE DELLA TERRA, UNIVERSITA DI FIRENZE, VIA G LA PIRA 4, 50121 FIRENZE, ITALY

Aims and Scopes

The journal OFIOLITI focuses on the geological study of ophiolites and related tectonic processes, contributing significantly to our understanding of oceanic crust formation, subduction dynamics, and the evolution of ancient oceanic environments. Its core areas include:
  1. Ophiolite Studies:
    The journal emphasizes detailed investigations of ophiolitic complexes, which are fragments of oceanic crust and upper mantle that have been thrust onto continental margins. This includes studies on their geochemistry, mineralogy, and structural geology.
  2. Geochronology and Isotope Geochemistry:
    A significant focus is on dating geological formations and understanding their evolution through isotopic studies. This involves the application of U-Pb, Nd-Sr-Pb isotope systematics to unravel the history of ophiolites and associated geological features.
  3. Paleoceanography and Biostratigraphy:
    Research in this journal often includes the examination of radiolarians and other microfossils to establish biostratigraphic frameworks, providing insights into past oceanic conditions and tectonic settings.
  4. Fluid-Rock Interaction and Alteration Processes:
    The journal publishes studies on the alteration of peridotites and other rock types, focusing on processes such as carbonatization, silicification, and serpentinization, which are crucial for understanding the geochemical cycles and the role of fluids in geological settings.
  5. Tectonic and Structural Geology:
    Research often investigates the tectonic evolution of regions containing ophiolites, including the study of deformation mechanisms, accretionary processes, and the implications for plate tectonics.
Recent years have seen a notable evolution in the themes published in OFIOLITI, with emerging trends reflecting the journal's adaptation to current scientific inquiries and technological advancements. These include:
  1. Carbon Capture and Storage Research:
    There is a growing interest in the role of ophiolites in carbon sequestration, particularly through the study of carbonatization processes in peridotites, indicating a response to global concerns about climate change and CO2 management.
  2. Hydrothermal Systems and Mineralization:
    Research focusing on hydrothermal processes associated with ophiolitic settings is on the rise, emphasizing the economic significance of these systems and their role in the formation of mineral deposits.
  3. Geochemical Variability and Environmental Impacts:
    Studies examining local geochemical variability in relation to environmental conditions and their implications for groundwater systems are becoming more prominent, showcasing the intersection of geology with environmental science.
  4. Interdisciplinary Approaches:
    There is an increasing trend towards interdisciplinary studies that integrate geology with other fields such as geochemistry, hydrology, and environmental science, reflecting a holistic approach to understanding complex geological systems.

Declining or Waning

While OFIOLITI has a robust focus on various geological aspects, certain themes appear to be waning in frequency or prominence in recent publications. These include:
  1. Continental Margin Sedimentology:
    Research specifically focused on sedimentological processes at continental margins has decreased, possibly due to a shift towards more focused studies on ophiolitic complexes rather than broader sedimentary contexts.
  2. Paleomagnetism:
    The application of paleomagnetic studies to understand the tectonic history of ophiolites and surrounding regions seems to be less frequent, indicating a potential decline in interest or available research in this area.
  3. Volcanic Activity Studies:
    While volcanic activity is still a relevant topic, specific studies focusing solely on volcanic sequences without a direct connection to ophiolitic contexts have diminished, reflecting a narrowing focus on ophiolite-related volcanism.

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