Add to ORKGThe main sources of diamond crystals (kimberlites, lamproites, etc.) are well known. The morphology of diamonds from impactites and metamorphic rocks is uncommon and less known. Metamorphic diamonds are known fro
Graphite cuboids are abundant in ultrahigh-pressure metamorphic rocks and are generally interpreted ...
In eastern Australia, diamonds occur in alluvial deposits overlying Phanerozoic basement. The origin...
Technical developments in analytical methods that reach nanometer spatial resolution have enabled th...
External and internal morphologies of natural impact apographitic diamonds (paramorphoses) have been...
The identification of syngenetic inclusions in diamond (i.e. inclusions of minerals that crystallize...
The identification of syngenetic inclusions in diamond (i.e. inclusions of minerals that crystallize...
A model for the genesis of natural diamond is presented based on the physical, chemical and mineralo...
Diamonds can form in a number of different ways. Physical and chemical properties of diamonds classi...
A genetic relationship between diamond and subcalcic Cr-pyrope garnet, both being produced by a meta...
A genetic relationship between diamond and subcalcic Cr-pyrope garnet, both being produced by a meta...
A variety of mantle-derived igneous rocks comprise the primary sources of diamond, with the principa...
The origin of diamonds in ureilite meteorites is a timely topic in planetary geology as recent studi...
More than 5,000 diamond crystals (or fragments) from kimberlite sills and placer deposits in the Gua...
Polished plates of diamondites (polycrystalline diamond aggregates) from Africa and in eclogites fro...
I studied a diamondiferous Archean meta-conglomerate from Wawa (North Ontario), part of the Michipic...
Graphite cuboids are abundant in ultrahigh-pressure metamorphic rocks and are generally interpreted ...
In eastern Australia, diamonds occur in alluvial deposits overlying Phanerozoic basement. The origin...
Technical developments in analytical methods that reach nanometer spatial resolution have enabled th...
External and internal morphologies of natural impact apographitic diamonds (paramorphoses) have been...
The identification of syngenetic inclusions in diamond (i.e. inclusions of minerals that crystallize...
The identification of syngenetic inclusions in diamond (i.e. inclusions of minerals that crystallize...
A model for the genesis of natural diamond is presented based on the physical, chemical and mineralo...
Diamonds can form in a number of different ways. Physical and chemical properties of diamonds classi...
A genetic relationship between diamond and subcalcic Cr-pyrope garnet, both being produced by a meta...
A genetic relationship between diamond and subcalcic Cr-pyrope garnet, both being produced by a meta...
A variety of mantle-derived igneous rocks comprise the primary sources of diamond, with the principa...
The origin of diamonds in ureilite meteorites is a timely topic in planetary geology as recent studi...
More than 5,000 diamond crystals (or fragments) from kimberlite sills and placer deposits in the Gua...
Polished plates of diamondites (polycrystalline diamond aggregates) from Africa and in eclogites fro...
I studied a diamondiferous Archean meta-conglomerate from Wawa (North Ontario), part of the Michipic...
Graphite cuboids are abundant in ultrahigh-pressure metamorphic rocks and are generally interpreted ...
In eastern Australia, diamonds occur in alluvial deposits overlying Phanerozoic basement. The origin...
Technical developments in analytical methods that reach nanometer spatial resolution have enabled th...