1979 - Member of the National Academy of Sciences
1975 - Fellow of John Simon Guggenheim Memorial Foundation
1973 - Fellow of American Geophysical Union (AGU)
His primary areas of study are Geochemistry, Mineralogy, Seawater, Great Oxygenation Event and Paleontology. His Geochemistry research is multidisciplinary, incorporating perspectives in Hydrothermal circulation and Organic geochemistry. His research integrates issues of Sulfide, Gneiss, Volumetric flow rate and Thermal energy in his study of Mineralogy.
His work carried out in the field of Seawater brings together such families of science as Environmental chemistry, Phanerozoic and Halite. His Phanerozoic research also works with subjects such as
His main research concerns Geochemistry, Mineralogy, Seawater, Earth science and Weathering. His work on Sedimentary rock and Great Oxygenation Event as part of general Geochemistry study is frequently connected to Paleosol, therefore bridging the gap between diverse disciplines of science and establishing a new relationship between them. His studies in Great Oxygenation Event integrate themes in fields like Paleoatmosphere and Isotopes of carbon.
His work deals with themes such as Metamorphism, Sulfate, Hydrothermal circulation and Dissolution, which intersect with Mineralogy. His biological study spans a wide range of topics, including Halite, Phanerozoic, Environmental chemistry and Evaporite. His studies deal with areas such as Earth, Carbon cycle and Physical geography as well as Earth science.
Heinrich D. Holland mainly investigates Geochemistry, Seawater, Mineralogy, Great Oxygenation Event and Paleontology. His Geochemistry study integrates concerns from other disciplines, such as Sulfate, Volume and Radiogenic nuclide. His research investigates the link between Seawater and topics such as Phanerozoic that cross with problems in Fluid inclusions, Evaporite, Halite and Paleozoic.
His Mineralogy research incorporates themes from Chlorite, Environmental chemistry, Geochemical cycle, Banded iron formation and Lithology. His Great Oxygenation Event study combines topics in areas such as Pyrite and Anoxic waters. While the research belongs to areas of Paleontology, Heinrich D. Holland spends his time largely on the problem of Sulfide, intersecting his research to questions surrounding Terrigenous sediment and Structural basin.
His primary scientific interests are in Great Oxygenation Event, Seawater, Geochemistry, Paleontology and Boring Billion. In Great Oxygenation Event, Heinrich D. Holland works on issues like Pyrite, which are connected to Organic matter, Carbon, Sulfur and Huronian glaciation. His Seawater research incorporates elements of Paleozoic, Dissolved silica, Phanerozoic, Environmental chemistry and Anhydrite.
His research in Geochemistry intersects with topics in Volume.remaining and Organic geochemistry. In general Paleontology, his work in Paleoatmosphere and Terrigenous sediment is often linked to Surface layer and Passive margin linking many areas of study. The Boring Billion study combines topics in areas such as Sulfur cycle, Sulfate, Isotopes of carbon and Weathering.
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Treatise on geochemistry
Heinrich D. Holland;Karl K. Turekian.
(2014)
The chemical evolution of the atmosphere and oceans
Heinrich D. Holland.
(1984)
The chemistry of the atmosphere and oceans
Heinrich D. Holland.
(1978)
The oxygenation of the atmosphere and oceans
Heinrich D Holland.
Philosophical Transactions of the Royal Society B (2006)
Dating the rise of atmospheric oxygen
A. Bekker;H. D. Holland;P.-L. Wang;D. Rumble.
Nature (2004)
Volcanic gases, black smokers, and the great oxidation event
Heinrich D. Holland.
Geochimica et Cosmochimica Acta (2002)
Chemical evolution of seawater during the Phanerozoic: Implications from the record of marine evaporites
Juske Horita;Heide Zimmermann;Heinrich D. Holland.
Geochimica et Cosmochimica Acta (2002)
Geochemistry of ∼1.9 Ga sedimentary rocks from northeastern Labrador, Canada
Ken-Ichiro Hayashi;Hiroyuki Fujisawa;Heinrich D. Holland;Hiroshi Ohmoto;Hiroshi Ohmoto.
Geochimica et Cosmochimica Acta (1997)
The evaporation path of seawater and the coprecipitation of Br- and K+ with halite.
M. A. McCaffrey;B. Lazar;H. D. Holland.
Journal of Sedimentary Research (1987)
The co-precipitation of cations with CaCO3—IV. The co-precipitation of Sr2+ with aragonite between 16° and 96°C
David J.J Kinsman;H.D Holland.
Geochimica et Cosmochimica Acta (1969)
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