Re: FW: [iagi-net-l] Caltex
Kalau pengurangan pegawai gini sistemnya offering atau paksaan sih? kalau offering kan ditawarkan siapa yang mau keluar bisa mengambil paket... kalau paksaan kan yang ditunjuk mau enggak mau harus mengambil paket... kalau sistemnya paksaan apa saja ya pertimbangan management...? apakah melihat core bisnis atau tidak, lama bekerja, jenis pekerjaan atau malah besar kecilnya gaji... Denger - denger dulu waktu Arco malah banyak yang sukarela ngambil paketsudah punya tabungan dari paket lalu bisa nyambi kerja freelance di luar dengan gaji dolar... Rovicky Dwi Putrohari [EMAIL PROTECTED] 30/09/2003 12:11 PM Please respond to iagi-net To: [EMAIL PROTECTED], [EMAIL PROTECTED], [EMAIL PROTECTED] cc: Subject:FW: [iagi-net-l] Caltex Siapa tahu ada yang belum dengar... - - - - Caltex Pacific Indonesia to offload a quarter of its staff Alfean Hardy, Malaysia Tuesday, September 30, 2003 PT Caltex Pacific Indonesia will begin to lay off over a quarter of its workforce come October as part of a rationalisation program. The company is currently awaiting final approval from the country's Oil and Gas Executive Board (BP Migas) before it starts letting ago an expected 6,700 workers. A company official, Poedyo Oetomo, has confirmed that all the proper procedures have been adhered to and that the retrenchments are part of the company's rationalisation program brought about by the decline in operational areas and falling production levels from old wells. Oetomo believes that this move is a necessity if Caltex Pacific is to remain competitive in the coming years. == end quote rdp: Buat temen-temen di CPI tentunya hal ini menjadikan sesuatu seperti acara tivi H2C (harap-harap cemas). Tapi mungkin ngga perlu cemas, wong kita saat ini sedang berada di era yang serba cepat berubah musti berani dan yakin dapat menghadapi hal-hal sperti ini. Emang sih bagi beberapa orang tenang-tenang saja, Tetapi saya pernah denger ada juga temen yg cukup stress menghadapinya. Lah ya jarang yg punya pengalaman ttg hal ini :( Sharing, yuuk ..! Lagi-lagi sharing pengalaman yg saya harapkan. Buat temen-temen yg pernah mengalaminya baik ex MOI, ex VICO, ex ARCO dll yg pernah menghadapi mungkin dapat memberikan sumbangan pikiran bagaimana caranya melewati fase-fase H2C ini ... Tentunya temen-temen di CPI masih buanyak yang ingin terus bekerja kan ? Maksudku masih belum pingin pensiun kan Adakah men-temen di milisi ini yg mempunyai kiat-kiat supaya tetep dapat terus bekerja ? tanpa membingungkan istri serta anak-anak kita yang sudah terbiasa dengan permanen employement status tentunya. dikit sharing dr saya (bagi yang ingin mencari tempat kerja baru). kerja di tempat baru tentunya persiapan utk : - membuat CV (curricullum Vitae), - mencari lowongan kerja, - menulis lamaran, - interview serta - bagaimana tawar-menawar gaji+fasilitas. Saya dulu pernah memfw bagaimana membuat CV (di fogri apa dimilis ini ya ? :), yang terpenting adalah bahwa anda mengetahui apa yang anda inginkan serta kelebihan apa yang anda miliki (selain kelebihan pesangon kali ya .. upst !!) ... juga pengalaman kerja apa yang bisa dijual ke perusahaan lainnya. Tentunya anda sendiri yang mengetahuinya. Seringkali seseorang mempunyai bebrapa kelebihan dalam bidang kerjanya, nah kalau saya sarankan anda memliki beberapa CV dan dijual ke perusahaan tertentu yang menjadi 'target' anda. Pengalaman saya dan beberapa temen yang lain, bahwa lamanya proses hiring ini bisa sangat bervariasi, namun kira-kira 3-6 bulan sejak anda diundang interview. Jadi kalau anda memang menginginkan bekerja lagi ditempat lain ya tentunya persiapannya mulainya secepat mungkin. Dan siap-siap saja untuk suantai dan rileks ketika anda menunggu hiring proccess ini. bisa uga bantu-bantu organisasi profesi yang anda ikuti (HAGI, IAGI, FOGRI, atau alumni dll) ... sekalian meningkatkan networking anda Menurut pengalaman beberapa temen-temen yg saya temui menyatakan bahwa Networking ini sangat efektif dalam mencari kerja KKN ? ... mboh ach !!! aku cuman kasih tahu ini sebagai 'silaturahmi' saja :) Nah alternatif lain bisa juga menjadi konsultan lepass ...!! freelance consultant kalo ini tanya kang Andang yg sudah banyak makan 'rendang serta gudeg'-nya ... (ngga cuman asam-garam ... hiks hiks ..:) Aku yakin temen-temen lain banyak yg bisa ikutan sharing termasuk sharing lowongan kerja ... Gut lak RDP tidak ada pengalaman, pengetahuan serta ilmu ini yang berguna ... kecuali ilmu atau pengetahuan dan pengalaman itu dibagi atau dishare - To unsubscribe, e-mail: [EMAIL PROTECTED] Visit IAGI Website: http://iagi.or.id IAGI-net Archive 1: http://www.mail-archive.com/iagi-net%40iagi.or.id/ IAGI-net Archive 2: http://groups.yahoo.com/group/iagi Komisi Sedimentologi (FOSI) : F.
RE: FW: [iagi-net-l] Re: korelasi geodinamik
Wah mantab dapat info dari filosof-filosof besar: Prof. Koesoema, Pak ade, Pak Awang. Saya senang dengan susunan dari beliau ketiga. Saya tambahkan data USGS updated 5-5-1999 dibawah (smoga tak kepanjangan). Gambar ada diinternetnya. Susunan ini relatif mirip dengan susunan diatas dan sedikit berbeda. Kok 7 lapis batuan bumi ya gambar disana ? Dari data Pak Ade, dan dengan asumsi 70 % laut, 30 % darat, lalu kami hitung presentasi ketebalan, dan menjadi berturut-turut : Nama lapisan, Avrg. batas bawah lapisan dari surface(km), Avg. tebal (km), Presentasi ketebalan terhadap jejari Bumi (%), elatisistas : 1.Crust ( 13, 13, 0.2, solid) 2.Listhoferic mantle( 116, 103, 1.6, solid) 3.Asthenospher ( 250, 134, 2.1, ductile) 4.Tansition Zone ( 400, 150, 2.4, solid) 5.Lower Mantel (2900, 2500, 39.2, solid) 6.Outer core(5100, 2200, 34.5, liquid) 7.Inner core(6378, 1278, 20.0, solid) Lithosfere adalah Crust dan Listhoferic mantel (2 % dari jejari bumi) Mantel : Lower mantel, transition zone, asthenosfer, listhoferic mantel. Core : inner core, dan outer core. Bagaimana dengan susunan baru itu ? Tentu banyak variasi susunan lain. Salam, Maryanto. http://geology.about.com/gi/dynamic/offsite.htm?site=http%3A%2F%2Fpubs.usgs. gov%2Fpublications%2Ftext%2Finside.html Inside the Earth The size of the Earth -- about 12,750 kilometers (km) in diameter-was known by the ancient Greeks, but it was not until the turn of the 20th century that scientists determined that our planet is made up of three main layers: crust, mantle, and core. This layered structure can be compared to that of a boiled egg. The crust, the outermost layer, is rigid and very thin compared with the other two. Beneath the oceans, the crust varies little in thickness, generally extending only to about 5 km. The thickness of the crust beneath continents is much more variable but averages about 30 km; under large mountain ranges, such as the Alps or the Sierra Nevada, however, the base of the crust can be as deep as 100 km. Like the shell of an egg, the Earth's crust is brittle and can break. Cutaway views showing the internal structure of the Earth. Below: This view drawn to scale demonstrates that the Earth's crust literally is only skin deep. Below right: A view not drawn to scale to show the Earth's three main layers (crust, mantle, and core) in more detail (see text). Below the crust is the mantle, a dense, hot layer of semi-solid rock approximately 2,900 km thick. The mantle, which contains more iron, magnesium, and calcium than the crust, is hotter and denser because temperature and pressure inside the Earth increase with depth. As a comparison, the mantle might be thought of as the white of a boiled egg. At the center of the Earth lies the core, which is nearly twice as dense as the mantle because its composition is metallic (iron-nickel alloy) rather than stony. Unlike the yolk of an egg, however, the Earth's core is actually made up of two distinct parts: a 2,200 km-thick liquid outer core and a 1,250 km-thick solid inner core. As the Earth rotates, the liquid outer core spins, creating the Earth's magnetic field. Not surprisingly, the Earth's internal structure influences plate tectonics. The upper part of the mantle is cooler and more rigid than the deep mantle; in many ways, it behaves like the overlying crust. Together they form a rigid layer of rock called the lithosphere (from lithos, Greek for stone). The lithosphere tends to be thinnest under the oceans and in volcanically active continental areas, such as the Western United States. Averaging at least 80 km in thickness over much of the Earth, the lithosphere has been broken up into the moving plates that contain the world's continents and oceans. Scientists believe that below the lithosphere is a relatively narrow, mobile zone in the mantle called the asthenosphere (from asthenes, Greek for weak). This zone is composed of hot, semi-solid material, which can soften and flow after being subjected to high temperature and pressure over geologic time. The rigid lithosphere is thought to float or move about on the slowly flowing asthenosphere. http://geology.about.com/library/weekly/aa081599a.htm Getting to the Core The Century in Review: It took years of ingenious work A hundred years ago, science barely knew that the Earth even has a core. Today, we are tantalized by the details we know about the core and its connections with the rest of the planet. In fact, I think it's the start of a golden age of core studies. We knew by the 1890s, from the way the Earth rocks in response to the gravity of the Sun and Moon, that the planet has a heavy core, of the density of iron. In 1906 an early seismologist, Richard Dixon Oldham, determined that earthquake waves move through the central part of the Earth much slower than through the mantle around it. This is because the center is liquid. He discovered the
RE: [iagi-net-l] Re: korelasi geodinamik
Mungkin kepanjangan, sehingga kami kirim kembali diperpendek (smoga gag dobel terkirim). Berapa kata terpanjang bisa terkirim ? MYT -Original Message- From: Maryanto Sent: Tuesday, September 30, 2003 11:03 Pagi To: '[EMAIL PROTECTED]' Subject: RE: FW: [iagi-net-l] Re: korelasi geodinamik Wah mantab dapat info dari filosof-filosof besar: Prof. Koesoema, Pak ade, Pak Awang. Saya senang dengan susunan dari beliau ketiga. Saya tambahkan data USGS updated 5-5-1999 dibawah (smoga tak kepanjangan). Gambar ada diinternetnya. Susunan ini relatif mirip dengan susunan diatas dan sedikit berbeda. Kok 7 lapis batuan bumi ya gambar disana ? Dari data Pak Ade, dan dengan asumsi 70 % laut, 30 % darat, lalu kami hitung presentasi ketebalan, dan menjadi berturut-turut : Nama lapisan, Avrg. batas bawah lapisan dari surface(km), Avg. tebal (km), Presentasi ketebalan terhadap jejari Bumi (%), elatisistas : 1.Crust ( 13, 13, 0.2, solid) 2.Listhoferic mantle( 116, 103, 1.6, solid) 3.Asthenospher ( 250, 134, 2.1, ductile) 4.Tansition Zone ( 400, 150, 2.4, solid) 5.Lower Mantel (2900, 2500, 39.2, solid) 6.Outer core(5100, 2200, 34.5, liquid) 7.Inner core(6378, 1278, 20.0, solid) Lithosfere adalah Crust dan Listhoferic mantel (2 % dari jejari bumi) Mantel : Lower mantel, transition zone, asthenosfer, listhoferic mantel. Core : inner core, dan outer core. Bagaimana dengan susunan baru itu ? Tentu banyak variasi susunan lain. Salam, Maryanto. http://geology.about.com/gi/dynamic/offsite.htm?site=http%3A%2F%2Fpubs.usgs. gov%2Fpublications%2Ftext%2Finside.html Inside the Earth The size of the Earth -- about 12,750 kilometers (km) in diameter-was known by the ancient Greeks, but it was not until the turn of the 20th century that scientists determined that our planet is made up of three main layers: crust, mantle, and core. This layered structure can be compared to that of a boiled egg. The crust, the outermost layer, is rigid and very thin compared with the other two. Beneath the oceans, the crust varies little in thickness, generally extending only to about 5 km. The thickness of the crust beneath continents is much more variable but averages about 30 km; under large mountain ranges, such as the Alps or the Sierra Nevada, however, the base of the crust can be as deep as 100 km. Like the shell of an egg, the Earth's crust is brittle and can break. Cutaway views showing the internal structure of the Earth. Below: This view drawn to scale demonstrates that the Earth's crust literally is only skin deep. Below right: A view not drawn to scale to show the Earth's three main layers (crust, mantle, and core) in more detail (see text). Below the crust is the mantle, a dense, hot layer of semi-solid rock approximately 2,900 km thick. The mantle, which contains more iron, magnesium, and calcium than the crust, is hotter and denser because temperature and pressure inside the Earth increase with depth. As a comparison, the mantle might be thought of as the white of a boiled egg. At the center of the Earth lies the core, which is nearly twice as dense as the mantle because its composition is metallic (iron-nickel alloy) rather than stony. Unlike the yolk of an egg, however, the Earth's core is actually made up of two distinct parts: a 2,200 km-thick liquid outer core and a 1,250 km-thick solid inner core. As the Earth rotates, the liquid outer core spins, creating the Earth's magnetic field. Not surprisingly, the Earth's internal structure influences plate tectonics. The upper part of the mantle is cooler and more rigid than the deep mantle; in many ways, it behaves like the overlying crust. Together they form a rigid layer of rock called the lithosphere (from lithos, Greek for stone). The lithosphere tends to be thinnest under the oceans and in volcanically active continental areas, such as the Western United States. Averaging at least 80 km in thickness over much of the Earth, the lithosphere has been broken up into the moving plates that contain the world's continents and oceans. Scientists believe that below the lithosphere is a relatively narrow, mobile zone in the mantle called the asthenosphere (from asthenes, Greek for weak). This zone is composed of hot, semi-solid material, which can soften and flow after being subjected to high temperature and pressure over geologic time. The rigid lithosphere is thought to float or move about on the slowly flowing asthenosphere. http://geology.about.com/library/weekly/aa081599a.htm The Century in Review: It took years of ingenious work A hundred years ago, science barely knew that the Earth even has a core. Today, we are tantalized by the details we know about the core and its connections with the rest of the planet. In fact, I think it's the start of a golden age of core studies. We knew by the 1890s, from the way the Earth rocks in response to the gravity of the Sun and Moon, that the planet
RE: FW: [iagi-net-l] Re: korelasi geodinamik
Hanya ingin koreksi sedikit, sebab cukup banyak yg melakukan kesalahan ini. Presentasi beda dg persentasi atau prosentase. Yg dimaksud di bawah tentunya adalah persentasi (atau prosentase) yg dilambangkan '%'. Maryanto [EMAIL PROTECTED] To: '[EMAIL PROTECTED]' [EMAIL PROTECTED] .comcc: bambang_dwiyanto [EMAIL PROTECTED], Herman Moechtar [EMAIL PROTECTED], Ukat Sukanta at CPI 09/30/03 11:02[EMAIL PROTECTED], 'Sardjono' [EMAIL PROTECTED], Indra AMBudiman (E-mail 2) [EMAIL PROTECTED] Please respond Subject: RE: FW: [iagi-net-l] Re: korelasi geodinamik to iagi-net Wah mantab dapat info dari filosof-filosof besar: Prof. Koesoema, Pak ade, Pak Awang. Saya senang dengan susunan dari beliau ketiga. Saya tambahkan data USGS updated 5-5-1999 dibawah (smoga tak kepanjangan). Gambar ada diinternetnya. Susunan ini relatif mirip dengan susunan diatas dan sedikit berbeda. Kok 7 lapis batuan bumi ya gambar disana ? Dari data Pak Ade, dan dengan asumsi 70 % laut, 30 % darat, lalu kami hitung presentasi ketebalan, dan menjadi berturut-turut : Nama lapisan, Avrg. batas bawah lapisan dari surface(km), Avg. tebal (km), Presentasi ketebalan terhadap jejari Bumi (%), elatisistas : 1.Crust ( 13, 13, 0.2, solid) 2.Listhoferic mantle ( 116, 103, 1.6, solid) 3.Asthenospher ( 250, 134, 2.1, ductile) 4.Tansition Zone( 400, 150, 2.4, solid) 5.Lower Mantel (2900, 2500, 39.2, solid) 6.Outer core (5100, 2200, 34.5, liquid) 7.Inner core (6378, 1278, 20.0, solid) Lithosfere adalah Crust dan Listhoferic mantel (2 % dari jejari bumi) Mantel : Lower mantel, transition zone, asthenosfer, listhoferic mantel. Core : inner core, dan outer core. Bagaimana dengan susunan baru itu ? Tentu banyak variasi susunan lain. Salam, Maryanto. http://geology.about.com/gi/dynamic/offsite.htm?site=http%3A%2F%2Fpubs.usgs . gov%2Fpublications%2Ftext%2Finside.html Inside the Earth The size of the Earth -- about 12,750 kilometers (km) in diameter-was known by the ancient Greeks, but it was not until the turn of the 20th century that scientists determined that our planet is made up of three main layers: crust, mantle, and core. This layered structure can be compared to that of a boiled egg. The crust, the outermost layer, is rigid and very thin compared with the other two. Beneath the oceans, the crust varies little in thickness, generally extending only to about 5 km. The thickness of the crust beneath continents is much more variable but averages about 30 km; under large mountain ranges, such as the Alps or the Sierra Nevada, however, the base of the crust can be as deep as 100 km. Like the shell of an egg, the Earth's crust is brittle and can break. Cutaway views showing the internal structure of the Earth. Below: This view drawn to scale demonstrates that the Earth's crust literally is only skin deep. Below right: A view not drawn to scale to show the Earth's three main layers (crust, mantle, and core) in more detail (see text). Below the crust is the mantle, a dense, hot layer of semi-solid rock approximately 2,900 km thick. The mantle, which contains more iron, magnesium, and calcium than the crust, is hotter and denser because temperature and pressure inside the Earth increase with depth. As a comparison, the mantle might be thought of as the white of a boiled egg. At the center of the Earth lies the core, which is nearly twice as dense as the mantle because its composition is metallic (iron-nickel alloy) rather than stony. Unlike the yolk of an egg, however, the Earth's core is actually made up of two distinct parts: a 2,200 km-thick liquid outer core and a 1,250 km-thick solid inner core. As the Earth rotates, the liquid outer core spins, creating the Earth's magnetic field. Not surprisingly, the Earth's internal structure influences plate tectonics. The upper part of the mantle is cooler and more rigid than the deep mantle; in many ways, it behaves like the overlying crust. Together they form a rigid layer of rock called the lithosphere (from
[iagi-net-l] Test Mohon Delete
Test, mohon delete. - To unsubscribe, e-mail: [EMAIL PROTECTED] Visit IAGI Website: http://iagi.or.id IAGI-net Archive 1: http://www.mail-archive.com/iagi-net%40iagi.or.id/ IAGI-net Archive 2: http://groups.yahoo.com/group/iagi Komisi Sedimentologi (FOSI) : F. Hasan Sidi([EMAIL PROTECTED])-http://fosi.iagi.or.id Komisi SDM/Pendidikan : Edy Sunardi([EMAIL PROTECTED]) Komisi Karst : Hanang Samodra([EMAIL PROTECTED]) Komisi Sertifikasi : M. Suryowibowo([EMAIL PROTECTED]) Komisi OTODA : Ridwan Djamaluddin([EMAIL PROTECTED] atau [EMAIL PROTECTED]), Arif Zardi Dahlius([EMAIL PROTECTED]) Komisi Database Geologi : Aria A. Mulhadiono([EMAIL PROTECTED]) -
RE: [iagi-net-l] Evolusi === Sudut pandang lain yoooook.
Jumlah famili dari spesies umur Ordovisian hingga kini (Data: Djoko T Iskandar, buku evolosi, ITB, 2000) mempunyai korelasi sangat bagus dengan Grafik Salam. Belum kami hitung angka korelasinya, tapi melihat trendnya bisa mendapatkan korelasi 90 %. Tak ada pengukuran tanpa error, begitu juga kedua kurva tadi. Keteraturan siklus pada Salam, lebih memungkinkan ketelitian yang lebih baik. Grafik itu adalah siklus order1, 700 Ma pereode dominantnya. Jumlah spesies itu pada umur Ma : 400, 400 ; 250, 225; 500, 0. Disitu sesuai dengan Permian extinction, Cretaceus extinction, matinya dinosaurus. Korelasinya, bila kompresi, dingin, maka jumlah famili sedikit, sebaliknya, extention kontinental, hangat, maka jumlah families bertambah. Mungkin ini masih pada temperatur dibawah Best life Temperatur semuanya. Kurva siklus nano plangkton (NN) pada skala umur geologi itu, mungkin sebagai orde 3 (atau 4) definisi orde pada hipotesa Salam. Apakah ada grafik-garfik flora-fauna detil lagi, misal juga umur homosapiens, siapa yang punya ? Evolusi yang saya pikirkan kini: semua benda adalah dari hidogen atom ber elektron 1 dimulai waktu big-bang, menjadi yang paling bisa mengatur diri, manusia. Netter: ma'af banyak terulang kami kirim pada re: korelasi geodinamik kemarin. Salam, Maryanto. From: Awang Satyana [EMAIL PROTECTED] Date: Tue Sep 2, 2003 8:30 am Subject: RE: [iagi-net-l] Evolusi === Sudut pandang lain yok. Itu hanya penyalahgunaan teori evolusi untuk kepentingan pribadi (c.q. rasialisme). Menulis novel semacam ini pun menurut saya muatan SARA-nya besar sekali. Kenapa hidung2 orang Eropa mancung dan lubangnya seperti celah karena katanya mereka hidup di daerah dingin, udara yang dingin perlu masuk berliku2 di ruang sempit (kan mancung) sehingga terjadi pemanasan dan pada saat masuk ke paru-paru sudah cukup hangat. Kenapa lubang hidung orang Asia lebih bulat karena katanya udara di daerahnya sudah panas, tidak perlu pemanasan tambahan di hidung, berilah yang bulat biar udara langsung masuk ke paru-paru dengan lancar. Kenapa ras mongolid matanya sipit dan kelopak matanya tebal karena katanya mereka hidup di perbatasan Gurun Gobi dengan anginnya yang kencang dan membawa pasir, tentu saja mata butuh perlindungan tambahan. Di atas itu sebagian keterangan dari Human Geography, dan itu bukan evolusi. Ras Eropa tidak lebih tinggi daripada ras suku2 di Afrika. Bahkan kalau percaya teori evolusi-antropologi out of africa, maka orang2 Eropa diturunkan dari nenek moyang Africa di sepanjang (East African Rift System). Neanderthal yang katanya nenek moyang orang Eropa berasal dari Pithecines Afrika. Jadi, harusnya orang Afrika mereka hormati, bukan diburu2. Ah sekedar novel...tapi novel sara. Salam, Awang H. Satyana Eksplorasi BP Migas - To unsubscribe, e-mail: [EMAIL PROTECTED] Visit IAGI Website: http://iagi.or.id IAGI-net Archive 1: http://www.mail-archive.com/iagi-net%40iagi.or.id/ IAGI-net Archive 2: http://groups.yahoo.com/group/iagi Komisi Sedimentologi (FOSI) : F. Hasan Sidi([EMAIL PROTECTED])-http://fosi.iagi.or.id Komisi SDM/Pendidikan : Edy Sunardi([EMAIL PROTECTED]) Komisi Karst : Hanang Samodra([EMAIL PROTECTED]) Komisi Sertifikasi : M. Suryowibowo([EMAIL PROTECTED]) Komisi OTODA : Ridwan Djamaluddin([EMAIL PROTECTED] atau [EMAIL PROTECTED]), Arif Zardi Dahlius([EMAIL PROTECTED]) Komisi Database Geologi : Aria A. Mulhadiono([EMAIL PROTECTED]) -
