> Awang

  Terima kasih atas informasi-nya , karena kalau Sioarjo ada s.z wah
  berabe dong.

  Si-Abah.

  ___________________________________________________________________

  Abah,
>
>   Dalam kasus LUSI, lumpur dan gas yang tersembur itu bukan merupakan
> akumulasi yang berasal dari sedimen yang terperangkap di zone subduksi
> seperti ditulis jurnal tersebut. Kita tahu, lumpur dan gas itu berasal
> dari zone depresi Kendeng yang sedimennya diendapkan dengan sangat cepat
> sehingga memicu diapirisme, diapirisme memicu mud volcano, mud volcano
> tererupsi karena dipicu gempa atau kegiatan pemboran.
>
>   Tetapi, kalau untuk kasus gunung-gunung lumpur di Sawu Basin di utara
> Pulau Sawu (dekat Sumba-Rote), kalau Abah pernah lihat beberapa seismic
> sections di Sawu Basin, di situ banyak gunung2 lumpur bawah laut. Nah,
> ini adalah memang berasal dari sedimen yang terakumulasi di zone
> subduksi, dan erupsinya didorong oleh kompresi dari thrust sheets yang
> banyak terbentuk di melange wedge Sawu-Rote-Timor.
>
>   salam,
>   awang
>
>   [EMAIL PROTECTED] wrote:
>
>   Kang Awang.
>
> Re- keterangan diatas , bagaimana mengaplikasikan - nya dalam kasus
> Sidoarjo ?
>
> Apakah posisi subduction zone dan saat sedimentasi mendukung pendapat
> diatas ?
>
> Kelihatannya kita harus melihat dan belajar dari kejadian kejadian di -
> region lain untuk menambah data sebelum suatu kesimpulan final dicapai.
> Hal ini penting SEKALI karena akan menyangkut suatu keputusan Pengadilan
> dalam banyak "pengaduan dari masyarakat".
>
> Si- Abah
>
> [EMAIL PROTECTED] wrote:
>   > Coba kita tengok bagaimana jurnal-jurnal ilmiah luar negeri mengulas
> LUSI
>> ini. Saya mengamati beberapa, dan ternyata semua sama yaitu bahwa mereka
>> hanya sepakat bahwa Lusi adalah "mud volcano eruption" Apa penyebab
>> erupsinya ? Gempakah, pengeboran Lapindokah ? Tak tahu. Besar
>> kemungkinan
>> dua-duanya. Sebuah jurnal menyebutkan juga gejala geotermal. Di bawah
>> ini
>> adalah salah satunya.
>>
>> Salam,
>> Awang
>>
>>
>> Mud volcano floods Java
>>
>>
>> Disaster-plagued Indonesian island faces new threat.
>>
>> by Richard Van Noorden
>> [EMAIL PROTECTED]
>> What Has Happened ?
>> For 3 months a sea of hot mud has been gushing from the ground in
>> Sidoarjo, East Java, 35 kilometres south of Indonesia's second largest
>> city, Surabaya. The steaming mud pool is growing at an estimated 50,000
>> cubic metres a day, accompanied by hydrogen sulphide gas, and now
>> reportedly covers more than 25 square kilometres. The flow has not yet
>> been stopped; thousands of people have lost their homes.
>>
>> How bizarre... has this sort of disaster happened before?
>>
>> The Sidoarjo disaster is an example of a 'mud volcano'.
> ________________________________________________________________________
>
> Mud and gas
>> accumulates when sea sediments are trapped in subduction zones, where
>> one
>> tectonic plate slides under another, and can erupt out of volcanic cones
>> or simply from a crack in the ground.
>
> Kang Awang.
>
> Re- keterangan diatas , bagaimana mengaplikasikan - nya dalam kasus
> Sidoarjo ?
>
> Apakah posisi subduction zone dan saat sedimentasi mendukung pendapat
> diatas ?
>
> Kelihatannya kita harus melihat dan belajar dari kejadian kejadian di -
> region lain untuk menambah data sebelum suatu kesimpulan final dicapai.
> Hal ini penting SEKALI karena akan menyangkut suatu keputusan Pengadilan
> dalam banyak "pengaduan dari masyarakat".
>
> Si- Abah
>
> ________________________________________________________________________
>
>
>
> Mud volcanoes have burst on every
>> continent, but are abundant in the South Caspian region (offshore and
>> onshore Azerbaijan) and offshore Indonesia in the East Java Basin.
>> But the Sidoarjo mud volcano is rather unusual. It's huge. And, says Sam
>> Rice, a geologist at the University of Cambridge, UK, reports of the mud
>> eruption suggest that it is a hybrid between typical mud volcanoes and
>> hydrothermal vents. The mud is of an unusually high temperature (60 °C)
>> and contains enormously high concentrations of hydrogen sulphide gas.
>> This
>> suggests that some kind of volcanic, hydrothermal activity is going on
>> at
>> the same time.
>>
>> What creates the conditions for a mud volcano?
>>
>> Achim Kopf, a geologist from the University of Bremen, Germany, who has
>> studied mud volcanoes extensively, explains that marine sediment can be
>> scraped off an oceanic tectonic plate as it slides underneath a
>> continental plate. If the sediment accumulates rapidly and water is
>> trapped in its pores, this can stop the sediment being cemented by
>> pressure. The resulting reservoir of mud can be trapped underground. In
>> the case of the East Java mud flow, the mud is thought to have come from
>> a
>> reservoir some 2.7 kilometres below the Earth's surface.
>>
>> And what triggers an eruption?
>>
>> A number of things can create a crack that allows trapped mud to bubble
>> to
>> the surface; particularly earthquakes and drilling.
>>
>> And in Java specifically?
>>
>> In Java both of these things have happened recently. The oil and gas
>> exploration company PT Lapindo Brantas is drilling in the area, and the
>> gas and hot mud first spewed from the company's drilling rig on 28 May.
>> Geologist Georg Delisle of the Federal Institute for Geosciences and
>> Natural Resources (BGR), Hannover, Germany, explains that the drilling
>> apparently penetrated into the liquid sediment and created a connection
>> back to the surface. The pressure then squeezed up the mud, like
>> toothpaste from a tube. But it is likely that other connections were
>> made
>> to the surface, he adds not just through the drilling pipe because
>> attempts to pump concrete into the pipe to block the flow of mud have
>> failed.
>> On 27 May an earthquake struck and devastated Yogyakarta on Java, and
>> this
>> too could have cracked the ground, potentially helping to release the
>> mud.
>> But the quake's epicentre was some 300 kilometres away from the mud
>> volcano (making it only 2 on the Richter scale in that area).
>> The issue of what, exactly, caused this disaster is highly politically
>> charged. It is still under investigation by police, the government and
>> international experts.
>>
>> Just how big is the eruption?
>>
>> According to many geological experts, the scale of this mud volcano is
>> unprecedented at least on land.
>> In 1945, the Makran earthquake in Pakistan triggered the sudden
>> emergence
>> of three offshore mud volcanoes, and in March 1999 a mud volcano rose
>> out
>> of the water overnight to form Malan Island, 3 kilometres from
>> Pakistan's
>> coast. It is hard to estimate the volume of mud created by such
>> underwater
>> eruptions. And, notes Rice: "Because the extrusion of mud and toxic gas
>> occurs on the seabed it does not threaten human life and does not make
>> the
>> headlines."
>> 'Well-kick' the sudden surface eruption of gas and mud during offshore
>> oil
>> drilling is common, but usually stops after a few days. Delisle recalls
>> a
>> smaller-scale incident in the 1960s where a geothermal well in the
>> Wairakei geothermal field, New Zealand, ran wild: it took 3 months to
>> stop
>> the geothermal steam that found its way to the surface alongside the
>> original borehole.
>>
>> Can the disaster be stopped?
>>
>> Nobody knows. So far, nothing has worked. PT Lapindo Brantas's senior
>> vice-president Imam Agustino has been quoted saying: "The best-case
>> scenario [for stopping the mudflow] is now mid-November, but I have to
>> admit it might never be stopped."
>> Visit our newsblog to read and post comments about this story.
>> Article Copyright © 2006 MacMillan Publishers Ltd.
>> All rights reserved. This material may not be
>> published, broadcast, rewritten, or redistributed.
>>
>>
>
>
>
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-----  PIT IAGI ke 35 di Pekanbaru
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No. Rek: 123 0085005314
Atas nama: Ikatan Ahli Geologi Indonesia (IAGI)
Bank BCA KCP. Manara Mulia
No. Rekening: 255-1088580
A/n: Shinta Damayanti
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