Cherts and Siliceous Sediments Flashcards
(26 cards)
The general name for the siliceous sedimentary rocks.
Chert
What are the dominant minerals in a chert?
Quartz, Chalcedony, Opal
What are the minor minerals in a chert?
Clay minerals, Hematite, Dolomite, Organic Matter
Chert is commonly _________, deeper than CCD
Pelagic
True or False: Chert is host to petroleum, phosphorites, uranium, and manganese.
True
The types of quartz that comprises chert are:
MicroQuartz
MegaQuartz
Chalcedonic Quartz
Some minor chemical elements in cherts are derived from four possible sources, which are:
-Biogenic
-Detrital
-Hydrogenous
-Hydrothermal
It is a red colored chert, with trace amounts of hematite.
Jasper
A chert that resembles unglazed/ unpolished porcelain.
Porcellanite
Also known as nodular chert.
Flint
A chert that is interbedded chert and hematite, BIF
Jaspilite
A chert that is classified as dense and fine-grained
Novaculite
Has low density, is light colored, associated with hot springs and is an exploration marker
Siliceous Sinter
Cherts with crossbedding, laminations, ripple marks, sole marks, associated with siliceous ooze
Bedded Chert
The two types of Diatomaceous Deposits are:
Diatomaceous Chert - Lenses pieces of diatomites in silica cement
Diatomites - Light colored, soft, friable
Two types of Radiolarian Deposits are:
Radiolarian Chert - Well bedded, well developed, radiolarian fossils tend to survive diagenesis
Radiolarite - A bit harder than oozes
Is a result of inadequate examinations, or severe diagenesis
Bedded Chert with few to no skeletal remains
Cherts that are subspheroidal, masses, lenses, irregular layers, tan to black in color
Nodular Cherts
Solubility of silica/chert
At 25°C ~11ppm for quartz, 116ppm for amorphous silica
True or False: Silicic concentration in seawater is ~18 ppm
False, ~13 ppm
The only mechanism capable of large-scale silica extraction from undersaturated seawater
Removal of silica from ocean water by silica-secreting organisms to build opaline skeletal structures
Age of radiolarians
Cambrian/Ordovician to Holocene
Age of Diatoms
Jurassic –Holocene
Age of Silicoflagellates
Cretaceous –Holocene