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The isotopic constitution of sulphur in some stratiform lead-zinc sulphide ores
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What this work says
Outgoing claims: the papers this work cites, builds on, or argues with.
inferredcites →https://doi.org/10.1016/0016-7037(54)90036-8openalex-snapshot
The origin of native sulphur deposits from isotope fractionation studies
inferredcites →https://doi.org/10.1016/0016-7037(63)90074-7openalex-snapshot
The distribution and isotopic abundance of sulphur in recent marine sediments off southern California
inferredcites →https://doi.org/10.1016/0016-7037(63)90085-1openalex-snapshot
Schwefel-Isotopen-Untersuchungen am Pyrit-Sphalerit-Baryt-Lager Meggen/Lenne (Deutschland) und an verschiedenen Devon-Evaporiten
inferredcites →https://doi.org/10.1016/0016-7037(64)90085-7openalex-snapshot
Schwefelisotopen-untersuchungen an sulfiden aus den erzvorkommen der sierra de cartagena in Spanien
inferredcites →https://doi.org/10.1139/cjr49b-038openalex-snapshot
NATURAL VARIATIONS IN THE ISOTOPIC CONTENT OF SULPHUR AND THEIR SIGNIFICANCE
inferredcites →https://doi.org/10.1139/cjr50b-069openalex-snapshot
THERMODYNAMIC PROPERTIES OF ISOTOPIC COMPOUNDS OF SULPHUR
inferredcites →https://doi.org/10.2113/gsecongeo.54.3.374openalex-snapshot
Sulfur isotopes and hydrothermal mineral deposits
inferredcites →https://doi.org/10.2113/gsecongeo.54.4.588openalex-snapshot
Anomalous leads and the emplacement of lead sulfide ores
inferredcites →https://doi.org/10.2113/gsecongeo.55.1.73openalex-snapshot
Sulfur isotopes and ore deposits
inferredcites →https://doi.org/10.2113/gsecongeo.55.3.539openalex-snapshot
Geology, sulfur isotopes and the origin of the Heath Steele ore deposits, Newcastle, N. B., Canada
inferredcites →https://doi.org/10.2113/gsecongeo.55.8.1676openalex-snapshot
Sulfur isotopes and the origin of the sulfide deposits of the Bathurst-Newcastle area of northern New Brunswick
inferredcites →https://doi.org/10.2113/gsecongeo.56.6.1088openalex-snapshot
The stratigraphic succession and structure in the Zinc Corporation Ltd. and New Broken Hill Consolidated Ltd., Broken Hill, New South Wales
What points at this work
Incoming claims: where this work appears in other papers’ reference lists and arguments.
inferred← citeshttps://doi.org/10.1007/978-3-662-28603-6_44openalex-snapshot
Lead Isotope Measurements on Sediments from Atlantis II and Discovery Deep Areas
inferred← citeshttps://doi.org/10.1007/bf00201992openalex-snapshot
The deposition of volcanics and pyritite in the Iberian Pyrite Belt
inferred← citeshttps://doi.org/10.1007/bf00202543openalex-snapshot
Fluctuations in a magmatic sulphur isotope signature from the Pinnacles Mine, New South Wales, Australia
inferred← citeshttps://doi.org/10.1007/bf00207517openalex-snapshot
Minor element geochemistry of sulphide minerals in the Broken Hill Lode (N.S.W.) in relation to the origin of the ore
inferred← citeshttps://doi.org/10.1007/bf00207523openalex-snapshot
The Broken Hill ore body, Australia
inferred← citeshttps://doi.org/10.1007/s001260050220openalex-snapshot
The Iberian type of volcano-sedimentary massive sulphide deposits
inferred← citeshttps://doi.org/10.1016/0009-2541(95)00177-8openalex-snapshot
Stable isotope evidence for thermochemical sulfate reduction in the Dugald river (Australia) strata-bound shale-hosted zinclead deposit
inferred← citeshttps://doi.org/10.1016/0012-821x(69)90064-8openalex-snapshot
Experimental study of sulfur isotope fractionation between coexistent sulfide minerals
inferred← citeshttps://doi.org/10.1016/0016-7037(90)90207-2openalex-snapshot
A sulfur isotope study of pyrite genesis: The mid-proterozoic Newland formation, belt supergroup, Montana
inferred← citeshttps://doi.org/10.1016/0301-9268(95)00098-4openalex-snapshot
Origin of hydrothermal CuZnPb mineralisation in the Olary Block, South Australia: evidence from fluid inclusions and sulphur isotopes
inferred← citeshttps://doi.org/10.1016/b978-0-444-41401-4.50009-5openalex-snapshot
DEVELOPMENT OF SYNGENETIC IDEAS IN AUSTRALIA
inferred← citeshttps://doi.org/10.1016/b978-0-444-41401-4.50010-1openalex-snapshot
ORIGIN, DEVELOPMENT, AND CHANGES IN CONCEPTS OF SYNGENETIC ORE DEPOSITS AS SEEN BY NORTH AMERICAN GEOLOGISTS
inferred← citeshttps://doi.org/10.1016/b978-0-444-41402-1.50011-4openalex-snapshot
SULPHUR AND LEAD ISOTOPES IN STRATA-BOUND DEPOSITS
inferred← citeshttps://doi.org/10.1016/b978-0-444-41406-9.50016-6openalex-snapshot
THE McARTHUR ZINC–LEAD–SILVER DEPOSIT: FEATURES, METALLOGENESIS AND COMPARISONS WITH SOME OTHER STRATIFORM ORES
inferred← citeshttps://doi.org/10.1016/j.oregeorev.2003.11.001openalex-snapshot
Nature and origin of the fluids responsible for forming the Hellyer Zn–Pb–Cu, volcanic-hosted massive sulphide deposit, Tasmania, using fluid inclusions, and stable and radiogenic isotopes
inferred← citeshttps://doi.org/10.1016/s0166-1116(08)71065-3openalex-snapshot
Chapter 6.4 Biogeochemical Cycling of Sulfur
inferred← citeshttps://doi.org/10.1017/s0016756822000590openalex-snapshot
Zinc, sulfur and cadmium isotopes and Zn/Cd ratios as indicators of the origin of the supergiant Broken Hill Pb–Zn–Ag deposit and other Broken Hill-type deposits, New South Wales, Australia
inferred← citeshttps://doi.org/10.1017/s008045680001526xopenalex-snapshot
13.—Zoning of Ore Deposits: Types and Causes
inferred← citeshttps://doi.org/10.1029/rg006i002p00175openalex-snapshot
A model for the evolution of strontium and lead isotopes in a dynamic Earth
inferred← citeshttps://doi.org/10.1046/j.1400-0952.2003.01048.xopenalex-snapshot
Sulfur isotope distribution in Late Silurian volcanic‐hosted massive sulfide deposits of the Hill End Trough, eastern Lachlan Fold Belt, New South Wales
inferred← citeshttps://doi.org/10.1080/08120098508729328openalex-snapshot
Stable isotope, petrological, and fluid inclusion studies of minor mineral deposits from the McArthur Basin: Implications for the genesis of some sediment‐hosted base metal mineralization from the Northern Territory
inferred← citeshttps://doi.org/10.2343/geochemj.4.41openalex-snapshot
Seawater sulfate as a possible determinant for sulfur isotopic compositions of some strata-bound sulfide ores
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