Description

Our Geology product line includes instruments for geochemical analysis of kerogen-bearing and natural hydrogen source rocks, as well as equipment for thin-section preparation.

Kerogen source rock:
Kerogen source rocks are organic-rich sedimentary formations—such as shales, coals, marls, and organic-rich mudstones—that contain kerogen, the solid organic material responsible for generating oil and gas during burial and heating. These rocks are characterized by high concentrations of organic carbon, represented by Type I, II, or III kerogen, each with distinct hydrocarbon-generating potential. Through thermal cracking, kerogen breaks down to produce liquid and gaseous hydrocarbons, forming the foundation of conventional petroleum systems. Their evaluation typically relies on traditional Rock-Eval parameters such as S1, S2, TOC, and Tmax, which help assess source rock richness, quality, and maturity. Common examples of kerogen source rocks include marine and lacustrine shales, coal seams, and other organic-rich sedimentary deposits.
Vinci enables reliable kerogen source-rock characterization by providing not only integrated analytical tools that support TOC, S1–S2, and Tmax measurements, identify kerogen types, and improve maturity assessment, but also interpretation software such as GEOWORKS, a modular platform designed to process, integrate, and interpret geochemical and pyrolysis data for comprehensive subsurface evaluation—inviting you to explore our dedicated solutions.


Hydrogen source rock:
Hydrogen source rocks are geological formations capable of producing natural hydrogen (H₂), operating through mechanisms entirely different from traditional kerogen-based hydrocarbon systems. While organic-rich rocks can release small amounts of hydrogen when subjected to extreme heating, this process is marginal and not the primary focus of natural hydrogen exploration. Instead, the key contributors are inorganic or mineral hydrogen source rocks, which generate H₂ through water–rock reactions rather than organic decomposition. These processes include serpentinization of olivine-rich ultramafic rocks, oxidation–reduction reactions in iron-rich formations such as banded iron formations (BIFs), radiolysis of water in crystalline basement rocks, and other reactions involving Fe²⁺-bearing minerals. Collectively, these mineralogical and geochemical pathways form the foundation of modern natural hydrogen systems and guide current exploration strategies.
Vinci supports the evaluation of natural hydrogen source rocks by providing advanced analytical instruments that characterize mineralogical and geochemical pathways—such as serpentinization, iron redox reactions, and radiolysis—and by offering interpretation software like GEOWORKS, a modular platform designed to process, integrate, and interpret multi-parameter datasets for comprehensive H₂ system assessment, inviting you to explore our dedicated solutions.

Thin section tools
Thin-section products allow production of high-quality thin sections from a wide variety of materials for microscopic observation. The wide range of instruments available include either automated systems for numerous samples or manual systems for research laboratories.