Results 211 to 220 of about 139,956 (281)
Giant pit craters on the modern seafloor above magma-induced hydrothermal vent complexes of Scotia Sea, offshore Antarctica. [PDF]
Somoza L+6 more
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Tracking CO<sub>2</sub> migration and accumulation in the Subei Basin using geochronology and fluid inclusion quantitative analysis. [PDF]
Hu Y+9 more
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Optimizing blast design and bench geometry for stability and productivity in open pit limestone mines using experimental and numerical approaches. [PDF]
Deressa GW, Choudhary BS, Jilo NZ.
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2014
Sediments and sedimentary rocks form under natural process of physical, chemical and biological weathering of igneous, metamorphic and old sedimentary rocks. The mechanisms involve transpiration, deposition, compaction, lithification and/or diagnosis.
S.K. Haldar, Josip Tišljar
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Sediments and sedimentary rocks form under natural process of physical, chemical and biological weathering of igneous, metamorphic and old sedimentary rocks. The mechanisms involve transpiration, deposition, compaction, lithification and/or diagnosis.
S.K. Haldar, Josip Tišljar
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Evolution of Sedimentary Rocks
2003For almost a century, it has been recognized that the present-day thickness and areal extent of Phanerozoic sedimentary strata increase progressively with decreasing geologic age. This pattern has been interpreted either as reflecting an increase in the rate of sedimentation toward the present or as resulting from better preservation of the younger ...
J. Veizer, F.T. Mackenzie
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The Organization of Sedimentary Rocks
SEPM Journal of Sedimentary Research, 1950Attempted practical applications of existing classifications of sedimentary rocks commonly encounter difficulties and inconsistencies: (1) sediments normally unassociated during deposition are artificially grouped together; (2) inferences about environment, degree of tectonic influence, and other factors not everywhere legible in the rocks are required
Edward Charles Dapples+2 more
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