Hartwig E. Frimmel

ORCID: 0000-0003-3041-8208
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About
Contact & Profiles
Research Areas
  • Geological and Geochemical Analysis
  • Geochemistry and Geologic Mapping
  • Paleontology and Stratigraphy of Fossils
  • Geochemistry and Elemental Analysis
  • Geology and Paleoclimatology Research
  • earthquake and tectonic studies
  • High-pressure geophysics and materials
  • Geological and Geophysical Studies
  • Hydrocarbon exploration and reservoir analysis
  • Geological Studies and Exploration
  • Clay minerals and soil interactions
  • Geological formations and processes
  • Radioactive element chemistry and processing
  • Astro and Planetary Science
  • Metal Extraction and Bioleaching
  • Mineralogy and Gemology Studies
  • Planetary Science and Exploration
  • Crystal Structures and Properties
  • Mineral Processing and Grinding
  • Geological Modeling and Analysis
  • Mining Techniques and Economics
  • Pleistocene-Era Hominins and Archaeology
  • Methane Hydrates and Related Phenomena
  • Extraction and Separation Processes
  • Stellar, planetary, and galactic studies

University of Würzburg
2015-2024

University of Cape Town
2014-2023

V. B. Sochava Institute of Geography
2020

HeidelbergCement (Germany)
2020

Montanuniversität Leoben
2003

University of Vienna
1988

Abstract Neoproterozoic–Cambrian amalgamation of West Gondwana involved the collision several terranes older crust that are now in eastern South America and western Africa. U–Pb (SHRIMP) detrital zircon ages from representative metasedimentary units Ribeira Dom Feliciano belts (South America) Gariep Damara (Africa) provide constraints on possible sediment source areas across probable suture zones. zircons Palaeoproterozoic Archaean. For Belt, a contribution Meso- Neoproterozoic is present,...

10.1144/sp294.13 article EN Geological Society London Special Publications 2008-01-01

10.1016/j.epsl.2007.11.022 article EN Earth and Planetary Science Letters 2007-12-04

Dating of single zircons from low-grade metamorphosed rhyolites in the Rosh Pinah Formation Gariep Belt southwestern Namibia, using Pb evaporation technique, yielded a primary crystallization age . Both stratigraphic position and geochemistry volcanic rocks indicate an early continental rift environment. The new data not only provide for massive Zn-Pb-Cu sulfide mineralization associated with these rocks, but they also set maximum limit Neoproterozoic break-up southern Namibia. This is...

10.1086/629839 article EN The Journal of Geology 1996-07-01

The concept of the 4th industrial revolution is becoming a strategic determinant sustainability, success and competitiveness in modern mining sector. importance digital transformation industry has long been debated, hampered part by conservative nature Much debate focused on choosing suitable techniques that provide acceptable levels ore/waste selectivity, scale implementation, cost reduction metallurgical extraction techniques. purpose this review to give an overview minerals extractive...

10.1016/j.resourpol.2022.102851 article EN cc-by Resources Policy 2022-06-24

New U‐Pb zircon ages and geochemical data for felsic intrusive extrusive rocks from the Richtersveld Igneous Complex (RIC) related in westernmost part of 1.03–1.06‐Ga Namaqua‐Natal metamorphic belt, South Africa, indicate that this complex is not to post‐Namaqua orogenic collapse but product mantle‐derived alkaline magmatism an extensional stress field led breakup a Neoproterozoic supercontinent. The oldest age obtained crystallization granitic syenitic melts $$833\pm 2$$ Ma. Continued...

10.1086/320795 article EN The Journal of Geology 2001-07-01

Thousands of rounded particles fine-grained gold, released from a crossbedded gold specimen the Basal reef placer in Welkom field after acid digestion host quartz arenite, have revealed morphological features and abrasion textures that are characteristic detrital gold. The size range, which is between 0.038 0.473 mm, has lognormal distribution with mean 2.88 phi units (0.136 mm) standard deviation 0.48. This well-sorted sediment. shapes predominantly disclike toroidal forms being most...

10.2113/gsecongeo.88.2.237 article EN Economic Geology 1993-04-01

10.1016/j.earscirev.2018.03.011 article EN Earth-Science Reviews 2018-03-27
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