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All Journal TEKNIK Rotasi J@TI (TEKNIK INDUSTRI) El-HARAKAH : Jurnal Budaya Islam Geological Engineering E-Journal JSEH (Jurnal Sosial Ekonomi dan Humaniora) Jurnal Pendidikan Islam Jurnal Rekayasa Mesin Jurnal Geologi dan Sumberdaya Mineral (Journal of Geology and Mineral Resources) Ahkam: Jurnal Hukum Islam AL-IDARAH: JURNAL KEPENDIDIKAN ISLAM Jurnal Pendidikan Dasar Jurnal Sains Teknologi dan Lingkungan (JSTL) International Journal Pedagogy of Social Studies Al-Dzikra: Jurnal Studi Ilmu al-Quran dan al-Hadits Desimal: Jurnal Matematika Syntax Literate: Jurnal Ilmiah Indonesia Kinerja: Jurnal Ekonomi dan Manajemen Seminar Nasional Teknologi Informasi Komunikasi dan Industri MITRA: Jurnal Pemberdayaan Masyarakat Martabe : Jurnal Pengabdian Kepada Masyarakat JURNAL PENDIDIKAN TAMBUSAI EduReligia : Jurnal Pendidikan Agama Islam YUME : Journal of Management PengabdianMu: Jurnal Ilmiah Pengabdian kepada Masyarakat Jurnal Review Pendidikan dan Pengajaran (JRPP) JAIM (Jurnal Abdi Masyarakat) Jurnal InTent: Jurnal Industri dan Teknologi Terpadu SOLUSI JAS (Jurnal Agri Sains) Jurnal Ilmiah Profesi Pendidikan Al-Ittijah : Jurnal Keilmuan dan Kependidikan Bahasa Arab Jurnal Abdi Insani Jurnal PORKES Jurnal Pengabdian Masyarakat Teknik JIIP (Jurnal Ilmiah Ilmu Pendidikan) Journal of Applied Science, Engineering, Technology, and Education Jurnal Pengabdian Masyarakat Khatulistiwa PAKAR Pendidikan Jurnal Bakti Masyarakat Indonesia Biofarm : Jurnal Ilmiah Pertanian Academia Open Hijai - Journal on Arabic Language and Literature Sophist Jurnal Sosial Politik Kajian Islam dan Tafsir Indonesian Community Service and Empowerment Journal (IComSE) Community Empowerment Al-Ulum: Jurnal Pendidikan Islam Jurnal Ilmiah Wahana Pendidikan Journal La Lifesci Journal La Multiapp Jurnal SIAR ILMUWAN TANI Jurnal Pengabdian kepada Masyarakat Bina Darma Jurnal Akutansi Manajemen Ekonomi Kewirausahaan (JAMEK) TARBAWY: Indonesian Journal of Islamic Education Agroteksos Journal of Education Research Indonesian Journal of Innovation Studies Journal of Ocean, Mechanical and Aerospace -science and engineering- (JOMAse) AKADEMIK: Jurnal Mahasiswa Ekonomi & Bisnis Al-Ulum: Jurnal Pendidikan Islam TRILOGI: Jurnal Ilmu Teknologi, Kesehatan, dan Humaniora Jurnal Manajemen Stratejik dan Simulasi Bisnis Balance : Jurnal Akuntansi dan Manajemen Edukasia: Jurnal Pendidikan dan Pembelajaran Lamahu: Jurnal Pengabdian Masyarakat Terintegrasi Jurnal Pengabdian Masyarakat Bhinneka Journal of Artificial Intelligence and Digital Business International Journal of Engineering Continuity Eduvest - Journal of Universal Studies SERVIRISMA: Jurnal Pengabdian kepada Masyarakat AL ULYA: JURNAL PENDIDIKAN ISLAM Journal Markcount Finance Journal of Educational Management Research Sabangka Abdimas Jurnal Pengabdian Masyarakat Sabangka Jurnal Pengabdian Masyarakat Berkarya Jurnal Akuntansi Syariah Jurnal Pengabdian Sosial Alfuad: Jurnal Sosial Keagamaan Jurnal Penelitian Pendidikan Indonesia Journal of Soil Quality and Management Al-Hukama: The Indonesian Journal of Islamic Family Law Agroland: Jurnal Ilmu-ilmu Pertanian Jurnal Keadaban: Jurnal Sosial dan Humaniora Proceeding Of International Conference On Education, Society And Humanity Jurnal Abdimas J-CEKI Jurnal Ekonomi, Manajemen, Akuntansi PESHUM Balance: Jurnal Ekonomi
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Journal : TEKNIK

GEOLOGI KAMPUS TEMBALANG Krisna H, Wahju; Fahrudin, Fahrudin
TEKNIK Volume 29, Nomor 2, Tahun 2008
Publisher : Diponegoro University

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (5845.905 KB) | DOI: 10.14710/teknik.v29i2.1940

Abstract

Geological conditions at Tembalang areas and surround, Semarang, as a Undulating – Hillockymorphological. That’s can be representation lithological and structural conditions. This surveysused the Geoelectrical sounding and combined with geological surface mapping. There are 15points sounding of Geoelectrical, after interpreted with geological surface mapping, can beconclusion the Breccias lithologic overlay on the upper of Limestones lithologic and finding thereverse fault in the part north of areas survey.
RANCANG BANGUN MODEL KOMPRESI DAN TARIK PERMODELAN SANDBOX DAN MANFAATNYA Fahrudin, Fahrudin; Asmarakandy, Dimas
TEKNIK Vol 36, No 1 (2015): (Juli 2015)
Publisher : Diponegoro University

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (925.523 KB) | DOI: 10.14710/teknik.v36i1.8391

Abstract

Permodelan sandbox dibuat dengan system tektonik konvergen dan divergen dengan menggunakan pergerakan satu sumbu. Permodelan ini bertujuan untuk membuat alat mesin sandbox yang bisa digunakan untuk penelitian dan pengajaran. Mesin berhasil dibuat dan sudah diujicobakan. Ujicoba dengan menggunakan satu lapisan pasir yang diambil dari Formasi Ngrayong. Percobaan selanjutnya dengan beberapa lapisan. Percobaan dilakukan dengan pengamatan yang meliputi pengamatan permukaan dan penampang verikal. Pengamatan yang aspek morfologi, kelurusan struktur, dan perkembangan sesar yang terbentuk. Hasil percobaan menunjukkan bahwa pembentukan morfologi sangat berkaitan dengan pembentukan sesar. Struktur sesar dengan pola forward propagating thrust faults. Sesar tersebut disebabkan imbrikasi. Lipatan yang terbentuk akibat mekanisme propagasi sesar.[Design of Compression and Extensional of the Sandbox Model and Its Benefit] Divergent and convergent tectonic sytem can be studied from the sandbox modelling. This model has a axis of movement. Sandbox models itends to study the progress of structural geology such as fault and fold. We successfully made machine of sandbox. This machine has basal detachment from duraluminum. Material for model is taken by loose sand from Ngrayong Formation. This experiment focused to observation about morphology in surface and thrust or backthrust in subsurface. This experiment has compression system. Result of model was that morphological sequences associated with fault sequences. Fault is formed to have the pattern of forward propagating thrust faults. It’s caused by imbricate thrust system. Folding is formed by the mechanism of fault propagation folding. 
MODEL DEFORMASI GETAS DI ZONA SESAR KALIGARANG (KGFZ) SEMARANG: STUDI AWAL PENGAMATAN MIKROSTRUKTUR MENGGUNAKAN METODE PETROGRAFI Fahrudin, Fahrudin; Winarno, Tri
TEKNIK Volume 33, Nomor 1, Tahun 2012
Publisher : Diponegoro University

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (663.362 KB) | DOI: 10.14710/teknik.v33i1.3787

Abstract

Brittle deformation at Kaligarang fault zone result strain changes. That strain is microstructure.Microstructures can see closely petrography. That observation include grain form, microcrack can form atcontact point like Hertzian and diagonal intragranular microcracks. Grain forms over angular, straight, andconcoidal. Grain of crystal or lithic fragments floating at matrik or cements. Microcrack growth does not onlydepend on stress, but also on temperature and chemical environment, especially of the fluid in the crack.
STUDI PALEOSEISMOLOGI AKIBAT BENCANA GEMPA BUMI DI ZONA SESAR KALIGARANG (KGFZ) DI SEMARANG Fahrudin, Fahrudin
TEKNIK Volume 34, Nomor 1, Tahun 2013
Publisher : Diponegoro University

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (5388.228 KB) | DOI: 10.14710/teknik.v34i1.4815

Abstract

Earthquake in the past can study with paleoseismology. Kaligarang fault zone will record the event ofearthquake and result the sediment. The metode of research is detail field mapping and field excavation.Evidence of paleoseismology in the filed, we find the sand boil and carbon materials. We find two location ofsand boil near with reverse faults. Sand boil to precipitate at unit B Kalibeng Formation. Phase tectonic tocause earthquake occure at late Miocene – Early Pliocene.
MEKANISME DEFORMASI, PERGERAKAN (SENSE SHEAR) DAN PERKEMBANGAN STRUKTUR DALAM PROSES DEFORMASI DUCTILE Fahrudin, Fahrudin
TEKNIK Volume 32, Nomor 2, Tahun 2011
Publisher : Diponegoro University

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (672.774 KB) | DOI: 10.14710/teknik.v32i2.1700

Abstract

The deformation mechanisme in ductile – transition zone show microfracture cataclasis activities,intracrystalline deformations, twinning, kinking, solid-sate diffusion creep, recovery and recrystallisation. Thatactivities to extend the sense shear indication. Sense shear can see i.e porfiroclast, mica fish, porfiroblast, veins,strain shadow, strain fringe and boudin. Commonly sense shear indications to get the form of ellipsoid geometry.That geometry experience to development the structure along progressive deformations process. Thedevelopment of inclusion and fabric also occur at that process.
STUDY OF THE PIEZOMETRIC SURFACE AND HYDROCOMPACTION AT CONFINED AQUIFER CAUSED THE LAND SUBSIDENCE IN SEMARANG Fahrudin, Fahrudin; Najib, Najib
TEKNIK Volume 32, Nomor 1, Tahun 2011
Publisher : Diponegoro University

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (480.405 KB) | DOI: 10.14710/teknik.v32i1.1682

Abstract

Semarang city has experienced of the land subsidence that be caused by intake groundwater in confined aquiferabundant. The land subsidence happened during range of time 20 years, it’s critical boundary so that result theenvironmental damage. Hence needed a study of cause of the land subsidence. This study aim to know theposition of piezometric surface and also explain the mechanism hydrogeology when happened the landsubsidence. The study of spreading aquifer has been done by the analysis of secondary data which is in the formof drilling log data, piezometric surface and soil mechanics test obtained from PLG (Environmental Center ofGeology) Bandung. Later then, between the land subsidence and piezometric surface be overlay becamezonation. From the data made a analysis of cause of the land subsidence. This aquifer has the land subsidence.The land subsidence explainable with the experienced phenomenon fact for example degradation of piezometricsurface at confined aquifer and process of hydrocompaction. That process influenced by two factors that areassess the pore number (e) and specific gravity (Gs). The degradation of piezometric surface formed the trapezeof water table until 20 m from sea level with the mean 0.7 - 1.1 m/year. Hydrocompaction cause the degradationof number of mean pore 0.145 - 0.5 and specific gravity 0.009 - 0.073 . The degradation of piezometric surfaceand process the hydrocompaction cause the fast of land subsidence around 0.5 - 1.75 cm/year.
Co-Authors A'yun, Fatihatul A.A. Ketut Agung Cahyawan W Aam Abdussalam, Aam Abda Abda Abdul Bashith Abdul Qodir Abdullah, Sirajudin H. Abhitah, Athallah Nabiel Aceng Kosasih, Aceng Achmad Faqihuddin ACHMAD, IRFAN ZINAT Adi Pranata, Mohammad Sofyan aditya, Aditya Purnadani Afandy, Arief Rahman Afian, Nanang Nur Afifi, A. Nawawi Alfan Afrinaldi, Rolly Agung Wibowo Agus Fakhruddin Agus Priyantoro Ahmad Shofiyuddin Ichsan Ahmad Syamsu Rizal, Ahmad Syamsu Ahyar Ahyar Ainul Yaqin, Ifandi, Ghazali, Ainurrohman, Muhamad Aji, Fabian Ismu Alfaini, Ainul Yaqin Alfionita, Feni Almaliki, Muh. Alwi Amarullah, Moh. Amelia, Ayu Amudin, Amudin Anter Venus Anton Anton Arif Alfiansyah Arifin, Agus Zainul Asep Kurnia Permana Asih Priyati Asrianti, Nadia Putri Asrin Asrin Asrof, Syahran Azmi, Afkarul Bakti, Lalu Arifin Aria Bambang Hari Kusumo Budhi Martana Bustan Choirunisa, Maria Choirunisa Citra Ningtyas Dadi Setiadi Damora Rhakasywi David, Jerico Dewi Nur Asih Dian Safitri Diana Ariana Diana Puspita Sari Diharto Dimas Asmarakandy Diraharja, Rifat Satrio Dusturia, Nida Dwi Pramita, Riska Dwi Supriyanto, Muhammad Sofyan Dwiyanto Joko Suprapto Dyah Ika Rinawati Edi Suresman Efendi, Jauhari Ega Naufal, Hanif Eko Budi Santoso Endis Firdaus, Endis Erna Hernawati, Erna Erny Erny, Erny Fadilah, Salwa Nur Fadlillah Rumanda Fahmi Abdillah Fajar Islamy, Mohammad Rindu Fajriya, Siti Fakhrurrozi, Pupu Fakhrurrozi, Pupu Fathoni, Ilham Fauzi, Ade Fikri Fauzi, Muhammad Ihsan Fauziah, Arum Febriana, Indah Karima Febriana, Miftakhul Jannah Firdausi, Jinnani Fitri Wahyuni Fitri, Maulidatul Fitriasih, Fitriasih Fitriyah Fitriyah Francisco, Jeremi Fuad Muhammad Fuzie Priatamphatie, Fuzie Garniwa, Nanang Ghazali, M. Ghufron, Moh. Idil Gunawan, Rizaldi Chandra Gustiawati, Resty Hadi Nugroho Hamdani, Moh. Ulil Absor Hamzah, Muhammad Fakhri Haqiqi, M. Deni Hendrayadi, Dedik Hery Heryanto Hidayat, Vicky Rosyid Hidayaturrohman, Qisthi Alhazmi Hopiana, Nida Husnah, Dalilatul I Gusti Made Kusnarta Ifandi Ifandi Iman, M. Kamilul Imawan, Yuli Indra Kusuma Irwansyah Irwansyah Isnaini, Putri Lailatul Istianah Istianah Jaenuri Jaenuri Jamaluddin Majid jannah, lailatul Januar Aziz Zaenurrohman Jeinanda, Vidia Puti Joko Tunggal Joko Wahyudiono Joshua Shima Juwariyah, Tatik Kafin, Achmad Kahfi, Nazih Sadatul Kallaba, Yulianti Khalaksita Amikani Asbella Khoiriyah, Binti Kiki Fatmala, Kiki Kosim, Mohammad Nanang Kusumo, Rayhan Suryo Lalu Sukardi, Lalu Lestari, Eka Dwi Lukmana, M. Arifudin Lukmana, Muhammad Arifudin M. Ridwan Hidayatulloh, M. Ridwan Mahardhika, Dhika Bayu Mahfudi, Mohammad Khoiri Mahrup Mahrup Mahrup, Mahrup Maman Abdurrahman Masruroh, Nuril MASYHUR, AHMAD Maulita, Sintia Putri Mawaddah, Ida Ma’ali, Izzul Mia Rhianti, Ghefira Mirasari, Titi Montreano, Donny Muhamad Ali Muhamad Parhan Muhammad Ridwan Muhammad Ridwan Hidayatulloh, Muhammad Ridwan Muhammad Roehil Amin, Ayatullah,, Mochammad Sofyan Dwi, Dimas Hidayatullah, Ghufron Shodiqin, Muhammad Sarjan Muhammad Subhan Muhammad Zaironi Muhlis, Nur Khozim Mukminah, Mukminah Mulya, Viona Santi Mulyadi, Henki Desri Mulyana Abdullah Mulyana, Arif Mulyati Munawar Rahmat Mundzir, Ali Murad, Murad Muslih Muslih Mustari, Muhammad Muthi’ah, Nadia Nabila Fajrina Noviana, Nabila Fajrina Nabilatus Sa'adah, Rashika Najib Najib Nasrulloh, Ilham Netriwati Novitasari, Ita Nur Cholis Nurhedi, Moh. Nurza, Ashfira Nurza, Ashfira Nurzati, Syarif Adhika Adhin Oktavitasari, Dini Padusug, Padusung Padusung Pramono, Setio Pranoto, Agus Pranoto, Agus Prasetyo Hadi Prasetyo, Eko Andi Priyambudi, Gathot Pudjihardjo Henarno Putri Pratiwi, Metalis Putri, Fadila Rahmatika Qomariyah, Nurul Ulfa Rachman, Muhammad Nanda Fatur Ramadhan, Muh Syahru Ratnasari, Iis Reda Rizal Rianda Dirkareshza Rica Rachmawati Ridha, Azhari Ali Rizal, Moh Syaiful Rizki Wahyu Yunian Putra Rohmaniati, Baiq Siti Romadhoni, Riyan Rusmawati Rusmawati, Rusmawati Sa'diyah, Iis Salamuddin, Ahmad Sari, Maula Sari, Retna Sarjan, M Savanti, Fisa Sa’adah, Rashika Nabilatus Seandi Taroreh, Bangkit Selvia, Siska Ita Sembiring, Rosali Colia Septin, Althearae Nira Septiyaningsih, Rina Setyowati, Wiwit Shadiqul W , K Shafa, Naura Shafiyullah, Alhadi Shakila, Nur Asri Shodiqin, Ghufron Shofi, Ahmad SHOLIHIN, MOH. Sidiq, Abdullatif Sigit Pradana Siti Saniah, Siti Sitorus, Henry Binsar Hamonangan Sitti Chaeriah Ahsan Soemeinaboedhy, I Nym Solly Aryza Sri Wahyuni Sugiarto S Sukartono Sukartono Sulasminingsih, Sri Sumarno, Ardawi Sunaika, Sunaika Sunarsih Sunarsih Sundussiyah, Sundussiyah Supriyadi Supriyadi Suryo, Taufik Hadi Susilowat, Lolita Endang Sutarya, Muhamad Farad Suwardji Suwoyo, Heru Syafei, Makhmud Syahruddin Hattab Syaifuddin, Ahcmad Syaiful Rizal Tajidan, Tajidan TATANG HIDAYAT, TATANG Taufik Hidayat Taupiqqurrahman Tedi Purbangkara Tengku Riza Zarzani N Tidar, Anisa Nava Tri Winarno Ummi Kulsum Wafiqah, Wafiqah Wahju Krisna H Wahju Krisna Hidajat Wahyuni, Tri Indah Warjono, Warjono Wawan Hermawan Wawan Hermawan Wibowo, Ardiyan Adhi Yahya, M. Wildan Bin H.M. Yuli Nurasri Zainal Abidin, Moh Ali Zainal Arifin Zainullah, M. Rizki Zuhdiyah Matienatul Iemaaniah