Tracing fault‐related fluids using in situ trace elements: A case study in Upper Cambrian dolostone in Gucheng area, Tarim Basin, NW China
- 16 February 2021
- journal article
- research article
- Published by Wiley in Geological Journal
- Vol. 56 (6), 3301-3313
- https://doi.org/10.1002/gj.4105
Abstract
No abstract availableKeywords
Funding Information
- National Natural Science Foundation of China (41902239)
This publication has 54 references indexed in Scilit:
- Thermal evolution and maturation of lower Paleozoic source rocks in the Tarim Basin, northwest ChinaAAPG Bulletin, 2012
- Accurate determinations of fifty-four major and trace elements in carbonate by LA–ICP-MS using normalization strategy of bulk components as 100%Chemical Geology, 2011
- Rare earth elements in mussel shells of the Mytilidae family as tracers for hidden and fossil high-temperature hydrothermal systemsEarth and Planetary Science Letters, 2010
- Evidence for cross formational hot brine flow from integrated 87Sr/86Sr, REE and fluid inclusions of the Ordovician veins in Central Tarim, ChinaApplied Geochemistry, 2008
- Structurally controlled hydrothermal dolomite reservoir facies: An overviewAAPG Bulletin, 2006
- Pervasive dolomitization with subsequent hydrothermal alteration in the Clarke Lake gas field, Middle Devonian Slave Point Formation, British Columbia, CanadaAAPG Bulletin, 2006
- Structural characteristics and petroliferous features of Tarim BasinChinese Science Bulletin, 2002
- Hydrothermal dolomite—a product of poor definition and imaginationSedimentary Geology, 2002
- Rare earth element geochemistry of dolomites in the Middle Devonian Presqu'ile barrier, Western Canada Sedimentary Basin: implications for fluid‐rock ratios during dolomitizationSedimentology, 1994
- Rare earth element fractionation in metamorphogenic hydrothermal calcite, magnesite and sideriteTschermaks Mineralogische und Petrographische Mitteilungen, 1992