Marble Bar Chert Member

It s a big thick chert.

Marble bar chert member.

The lithofacies of the marble bar chert member on the outcrop are characterized by centimeter scale beds of red grey white and rare black layers. We re right at the bottom. A paleomagnetic study of 261 discrete specimens collected from a 158 5 to 182 0 m section of the marble bar chert member revealed two distinct magnetic components lt. Here we report new evidence to suggest that haematite crystals in the jasper chert unit of the 3 46 gyr marble bar chert member mbc in the pilbara craton western australia probably nucleated.

The marble bar chert member dated between 3463 to 3454 ma thorpe et al 1992 is a world famous early archean unit with little metamorphism. Another specimen is marble bar chert of 3 5 ga warrawoona group member which is distributed at pilbara craton in western australia. Initial magnetic measurements of the whole core revealed that the black or red layers in the marble bar chert member display strong natural remanence magnetization. 1 a well bedded evenly and finely flat laminated lower section characterized by a conspicuous red white dark blue banded facies and prominent brecciated beds locally referred to as.

Gunflint chert specimens were collected from the locality of kakabeka falls near lake superior. It is composed of two very distinctive sub units. Marble bar has a hot desert climate köppen bwh with sweltering summers and warm winters. Red and white banded chert at marble bar pool in the east pilbara.

You can see the nice layering all through here right up over. The layers of red chert jasper contain up to 10. The town set a world record of most consecutive days of 100 f 37 8 c or above during a period of 160 days from 31 october 1923 to 7 april 1924. Geological mapping reveals that the 3460 million year old marble bar chert was deposited in a caldera setting across an area of at least 50 km x 30 km.

The marble bar chert of the archean proterozoic sedimentary sequence is only slightly metamorphosed. Most of the annual rainfall occurs in the summer. Sedimentological evidence indicates water depths exceeding 200 m. These yellowy rocks are the volcanic rocks that underly the marble bar chert and the black is the chert.

The archean biosphere drilling project abdp drilled a continuous 270 m long oriented core from the towers formation which includes the marble bar chert member 3456 1 3476 0 ma in the pilbara craton northwestern australia. Here we interpret the finely laminated thin bedded cherts mixed conglomeratic beds. Marble bar chert member is located at chinaman pool.