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Exploration

This is my World. Structures: Folds and Faults in West Kalimantan, Borneo. In the northern part of Kalimantan, a number of thrust and normal faults have been identified trending E-W. The thrust faults may be associated with Late Cretaceous melange formation and were rejuvanated in the Early Miocene. The normal faults were formed after Oligocene time, probably in the Early Miocene. Diamond in Kalimantan, Borneo, Indonesia. In 1984 Anaconda Indonesia Inc., together with PT Aneka Tambang, carried out ex...

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This is my World. Structures: Folds and Faults in West Kalimantan, Borneo. In the northern part of Kalimantan, a number of thrust and normal faults have been identified trending E-W. The thrust faults may be associated with Late Cretaceous melange formation and were rejuvanated in the Early Miocene. The normal faults were formed after Oligocene time, probably in the Early Miocene. Diamond in Kalimantan, Borneo, Indonesia. In 1984 Anaconda Indonesia Inc., together with PT Aneka Tambang, carried out ex...

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Exploration | randyweblog.blogspot.com Reviews

https://randyweblog.blogspot.com

This is my World. Structures: Folds and Faults in West Kalimantan, Borneo. In the northern part of Kalimantan, a number of thrust and normal faults have been identified trending E-W. The thrust faults may be associated with Late Cretaceous melange formation and were rejuvanated in the Early Miocene. The normal faults were formed after Oligocene time, probably in the Early Miocene. Diamond in Kalimantan, Borneo, Indonesia. In 1984 Anaconda Indonesia Inc., together with PT Aneka Tambang, carried out ex...

INTERNAL PAGES

randyweblog.blogspot.com

1

Exploration: December 2009

http://randyweblog.blogspot.com/2009_12_01_archive.html

This is my World. Structures: Folds and Faults in West Kalimantan, Borneo. In the northern part of Kalimantan, a number of thrust and normal faults have been identified trending E-W. The thrust faults may be associated with Late Cretaceous melange formation and were rejuvanated in the Early Miocene. The normal faults were formed after Oligocene time, probably in the Early Miocene. Subscribe to: Posts (Atom). Structures: Folds and Faults in West Kalimantan, B.

2

Exploration: Coal Carbonization Process

http://randyweblog.blogspot.com/2009/11/coal-carbonization-process.html

This is my World. Coal carbonization include the reform process with the state of anaerobic (without oxygen) at low temperatures 459-700 Celsius and at high temperatures produces 900-12000 Celsius and porous solid materials which are residues carbonization process called coke or charcoal and volatile gases (Tsai, 1980 ). In general, the solid material consists of semi-coke is formed from the coal that is not experiencing maturation and coke derived from coal that has undergone maturation. Rank or rank of...

3

Exploration: January 2009

http://randyweblog.blogspot.com/2009_01_01_archive.html

This is my World. How to Fix Stuck Pixel on LCD. If your LCD screen has a stuck a point on the screen that is always lit red, yellow, blue, green or white, it is usually due to distribution of liquid in the liquid crystal display (TFT LCD) problem. This can often be fixed, but not on dead pixel (black dot color). Nothing can do on dead pixel, but if the stuck pixel you have then try this hopefully works. Try running pixel fixing software. Turn off your computer's monitor. Display a black image, which wil...

4

Exploration: Shape, Structure, and Volcanism Activity of Gunung Kelimutu (Kelimutu Mount), Flores Island, Indonesia

http://randyweblog.blogspot.com/2009/11/shape-structure-and-volcanism-activity.html

This is my World. Shape, Structure, and Volcanism Activity of Gunung Kelimutu (Kelimutu Mount), Flores Island, Indonesia. This mountain is located in the Central Flores Island, Endeh District, also called Mount Geli or Mutu. It is at 1640 m above sea level. This mountain has 3 craters are: Tiwu Ata Mbupu, Tiwu Nua Muri Kooh Fai, Tiwu Ata Polo. Mount Kelimutu is belong to strato type volcano. Double crater Nua Tiwu Kooh Fai and Tiwu Ata Polo surrounded by a dike ring with “C” shape. It is ...According to ...

5

Exploration: Regional Tectonic of Timor Island, Indonesia

http://randyweblog.blogspot.com/2009/11/regional-tectonic-of-timor-island.html

This is my World. Regional Tectonic of Timor Island, Indonesia. Arc-continent collision between Eastern Sunda Arc (Banda Arc) and Southwest Australia continent formed the southern boundary of the tectonic elements. This collision zone is part of the evolutionary stages of young or early and more to resemble aspects of normal trench-arc system. Subscribe to: Post Comments (Atom). Diamond in Kalimantan, Borneo, Indonesia. Geology of Sulawesi Island, Indonesia. Regional Tectonic of Timor Island, Indonesia.

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This is my World. Structures: Folds and Faults in West Kalimantan, Borneo. In the northern part of Kalimantan, a number of thrust and normal faults have been identified trending E-W. The thrust faults may be associated with Late Cretaceous melange formation and were rejuvanated in the Early Miocene. The normal faults were formed after Oligocene time, probably in the Early Miocene. Diamond in Kalimantan, Borneo, Indonesia. In 1984 Anaconda Indonesia Inc., together with PT Aneka Tambang, carried out ex...

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