NI 43-101 Technical Report for the Julietta Project in Europe, Russia dated January 2003 (Q38495): Difference between revisions
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Property / addresses subject | |||
Property / addresses subject: Cretaceous Period / rank | |||
Normal rank | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: 1,750 to 1,900 metre thick sequence of Upper to Lower Cretaceous mafic to felsic volcanic and volcaniclastic | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: subvolcanic stocks and dykes related to episodes of Cretaceous volcanism are present in the succession. The | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: volcanic-volcaniclastic sequences ranging in age from Lower to Upper Cretaceous. The oldest, the Lower Cretaceous | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: Cretaceous. The oldest, the Lower Cretaceous lvaninsky Sequence, is subdivided into | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: Unconformably overlying the above units is the Lower Cretaceous Engterinsky Sequence, a 250 to 300 metre | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: unconformably upon the previous sequence. It comprises Lower Cretaceous amygdaloidal pyroxene-bearing andesite | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: 2003 youngest sequence, the Makinsky Sequence, is Upper Cretaceous in age and consists of rhyodacite tuffs | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: intrusive rocks range in age from Lower to Upper Cretaceous. There are four known ages of dykes and | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: porphyritic diorite dykes which are confined to the Lower Cretaceous lvaninsky Sequence and older sedimentary | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: from rhyolitic to dacitic in composition. An Upper Cretaceous age is assigned to these dykes. The youngest | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: are diorite dykes and stocks of the Upper to Lower Cretaceous Okhotsky Complex. In the Julietta area | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: the Bulat Caldera System, which is related to the Cretaceous volcanic activity. The caldera subsidence | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: margin, juxtapose the Jurassic sediments and the Cretaceous volcanic rocks. A domal feature, termed | |||
Property / addresses subject: Cretaceous Period / qualifier | |||
concept highlight: veins. The gold-silver mineralization at Julietta is Lower Cretaceous in age and is low temperature epithermal | |||
Property / addresses subject: Cretaceous Period / reference | |||
Property / addresses subject: Cretaceous Period / reference | |||
Property / addresses subject | |||
Property / addresses subject: Jurassic Period / rank | |||
Normal rank | |||
Property / addresses subject: Jurassic Period / qualifier | |||
concept highlight: a 1,600 metre thick succession of Upper to Lower Jurassic terrestrial sedimentary rocks. A variety | |||
Property / addresses subject: Jurassic Period / qualifier | |||
concept highlight: Cretaceous volcanism are present in the succession. The Jurassic sedimentary rocks may be subdivided into | |||
Property / addresses subject: Jurassic Period / qualifier | |||
concept highlight: area is a 650 to 750 metre thick succession of Lower Jurassic coarse grained siltstones and sandstones | |||
Property / addresses subject: Jurassic Period / qualifier | |||
concept highlight: overlying this sequence is a 250 metre thick Lower Jurassic sequence of interbedded siltstone and argillite | |||
Property / addresses subject: Jurassic Period / qualifier | |||
concept highlight: faults, which, at the caldera margin, juxtapose the Jurassic sediments and the Cretaceous volcanic rocks. | |||
Property / addresses subject: Jurassic Period / reference | |||
Property / addresses subject: Jurassic Period / reference | |||
Revision as of 20:56, 19 April 2023
an NI 43-101 Technical Report pulled from the GeoArchive collection
Language | Label | Description | Also known as |
---|---|---|---|
English | NI 43-101 Technical Report for the Julietta Project in Europe, Russia dated January 2003 |
an NI 43-101 Technical Report pulled from the GeoArchive collection |
Statements
1,750 to 1,900 metre thick sequence of Upper to Lower Cretaceous mafic to felsic volcanic and volcaniclastic
subvolcanic stocks and dykes related to episodes of Cretaceous volcanism are present in the succession. The
volcanic-volcaniclastic sequences ranging in age from Lower to Upper Cretaceous. The oldest, the Lower Cretaceous
Cretaceous. The oldest, the Lower Cretaceous lvaninsky Sequence, is subdivided into
Unconformably overlying the above units is the Lower Cretaceous Engterinsky Sequence, a 250 to 300 metre
unconformably upon the previous sequence. It comprises Lower Cretaceous amygdaloidal pyroxene-bearing andesite
2003 youngest sequence, the Makinsky Sequence, is Upper Cretaceous in age and consists of rhyodacite tuffs
intrusive rocks range in age from Lower to Upper Cretaceous. There are four known ages of dykes and
porphyritic diorite dykes which are confined to the Lower Cretaceous lvaninsky Sequence and older sedimentary
from rhyolitic to dacitic in composition. An Upper Cretaceous age is assigned to these dykes. The youngest
are diorite dykes and stocks of the Upper to Lower Cretaceous Okhotsky Complex. In the Julietta area
the Bulat Caldera System, which is related to the Cretaceous volcanic activity. The caldera subsidence
margin, juxtapose the Jurassic sediments and the Cretaceous volcanic rocks. A domal feature, termed
veins. The gold-silver mineralization at Julietta is Lower Cretaceous in age and is low temperature epithermal
a 1,600 metre thick succession of Upper to Lower Jurassic terrestrial sedimentary rocks. A variety
Cretaceous volcanism are present in the succession. The Jurassic sedimentary rocks may be subdivided into
area is a 650 to 750 metre thick succession of Lower Jurassic coarse grained siltstones and sandstones
overlying this sequence is a 250 metre thick Lower Jurassic sequence of interbedded siltstone and argillite
faults, which, at the caldera margin, juxtapose the Jurassic sediments and the Cretaceous volcanic rocks.
P97 (Deleted Property)
4530692:U56NX82R Property P97 not found, cannot determine the data type to use.
0 references