Edge Rewrite
// HTMLRewriter · presentation

This page was redesigned at the edge.

Cloudflare fetched the original article and streamed it through HTMLRewriter to apply an entirely new visual system without rebuilding the source page.

// request.cf · coarse context

A page that knows where it met you.

Only coarse request metadata is shown. This demo does not display or persist visitor IP addresses.

Country
US
Cloudflare location
CMH
Connection
HTTP/2
Language
Not provided

Ray ID: a26abf94cb4e2a7e

Jump to content

// Workers AI · dad joke modeWhat did Muva say to her cow? Muve over.

From Wikipedia, the free encyclopedia

The Muva is a term coined by E.H. Ackermann (1950)[1] for a folded supracrustal shallow water succession of quartzites and pelites in the Irumide Belt of Zambia. The "Muva" was first described by A. Gray (1930).[2]

The sequence is interpreted as a 1.8 billion year old shallow marine to coastal sequence which includes dunal deposits (aeolian), beach sands, offshore sand deposits and deeper water pelitic sediments. The alternation of quartzite-pelite successions was interpreted to record transgressive and regressive phases of a coastline along the southern margin of the Bangweulu Block. The presence of these types of rocks is also seen in areas that have undergone marine transgression.

In the western coastline of the Indian peninsula the Jurassic strata show this character of undergoing a submergence owing to crustal disturbance on the surface of the ocean floor and lead to the presence of marl with limestone in shallow water areas. Such effects are widely observed along the western coastline of India in parts of Saurashtra (Gujarat) and the Salt Range of Rajasthan.

References

[edit]
  1. Ackermann, E.H., 1950, Ein neuer Faltengurtel in. Nordrhodesien und seine tectonische Stellung im Afrikanishen grundgebirge. Geologische Rundschau, 38: 24-39
  2. Gray A. (1930) The correlation of the ore-bearing sediments of the Katanga and. Rhodesian Copperbelt. Economic Geology, 25, 783-801.