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Pelayanan akademik adalah layanan pendidikan yang berhubungan erat dengan mahasiswa meliputi kurikulum, RPS, rancangan mutu perkuliahan, praktikum, pembimbingan dan lain sebagainya. Pelayanan akademik menjadi terganggu karena belum adanya digitalisasi pelayanan yang dilakukan UIN SMH Banten. Oleh sebab itu, dibutuhkan aplikasi SIMIKA dalam mempermudah pelayanan akademik yang dilakukan ke mahasiswa. Sehingga pandemi bukan lagi menjadi alasan untuk tidak memaksimalkan layanan akademik yang dilakukan. Metode penelitian menggunaan mix methods. Dengan langkah awal dilakukan survey untuk mengetahui permasalahan yang ada di lapangan, kemudian dari masalah tersebut dicarikan solusi yang tepat. Selanjutnya dilakukan installasi Aplikasi, setelah aplikasi dilakukan Installasi kemudian Sosialiasi dan Kembali di survei apakah aplikasi tersebut sesaui dengan kebutuhan dari pengguna. Hasil penelitian menunjukkan bahwa nilai rata-rata jawaban responden terhadap 11 pertanyaan berkode dari item 1 sampai 11 memiliki nilai minimal 1 (sangat tidak setuju) dan nilai maksimal 5 (sangat setuju). Respon responden yang setuju dengan keberadaan Sistem Informasi Manajemen Fakultas Sains (SIMIKA) sebagai layanan akademik online tergambar dari nilai rata-rata (mean) keseluruhan sebesar 3,91. Sistem Informasi Manajemen Layanan ini hanya menggunakan aplikasi yang tersedia di Hosting, yaitu menggunakan Aplikasi HelpDeskz pada Costumer Support, sehingga dapat menghemat anggaran yang dikeluarkan dalam pembangunan system layanan. Kata kunci : Digital, Pelayanan Akademik

Analysis of a peak ground acceleration value and earthquake intensity in Banten Province has been carried out using historical earthquake data from 2008 to 2018. This research aims to describe a prone area of the earthquake. The specification of data was a magnitude > 5 SR and the depth 0-70 km. The Donovan method was used to analyze peak ground acceleration value and the earthquake’s intensity. According to the data obtained, 31 earthquake points with a maximum earthquake strength occurred on October 16, 2019, with a depth of 10 km and a magnitude of 6.48 SR. This earthquake was located in Ujung Kulon with coordinates -6.81 LS and 105.113 BT. Based on data analysis result was obtained a peak ground acceleration value and the intensity of earthquake maximum in The Pandeglang Regency with a peak ground acceleration value was 211.56 cm/s2, and intensity of scale VIII and a large risk level of three. While a peak ground acceleration minimum is located in the South Tangerang City was 62.82 cm/s2 with a scale of intensity VII and a moderate risk level.

Mapping of rock resistivity value is useful for knowing the potential of the natural wealth contained in the earth. Investigation of resistivity value in Solok Regency is using 3 lines. The first line is at S 00055'0.7 "and E 100040'56.8" coordinates, the second line is located at S 00054'53.2 "and E 100041'00.9" coordinates, and the third line is coordinated by S 00055'20.5 "and E 100041'01.8". The method of mapping is using the Geoelectric method with Schlumberger Configuration and the Ares (Apparent Resistivity) tool. The data obtained is processed by using Res2Dinv software to be analyzed and interpreted. The results obtained on the first line have resistivity value of 3.95-641 Ωm which is interpreted by having a rock structure consisting of Groundwater, Clay, Dry Clay, Basalt and Andesite. Next on the second line, the resistivity values of 2.53-1560.5 Ωm are obtained consisting of layers of rock Groundwater, Clay, Dry Clay, Basalt, and Andesite. Finally on the third line have resistivity value about 6.85-113.5 Ωm having a Groundwater, Tuff, Sandstone, Clay, Dry Clay, Basalt, Andesite, and Lava rock structure. The Tuff rock layer is estimated as a geothermal reservoir because its resistivity value is 20.8-23.6 Ωm surrounded by more contrasting rock layers and is located between two solid rock layers.

One-dimensional (1D) and two-dimensional (2D) magnetotelluric data inversion were conducted to reveal the subsurface resistivity structure beneath the eastern part of a volcano in Central Java, Indonesia. Fifteen magnetotelluric sounding data spanning two lines of investigation were inverted using Occam's inversion scheme. The result depict that there are extensively conductive layer (2-10 ohm meter) below the volcanic overburden. This conductive layer is interpreted as the clay cap resulted from thermal alteration. A higher resistivity layer (10-80 ohm meter) underlies the clay cap and is interpreted as the reservoir whose top boundaries vary between 1000 m above and 2000 m below sea level.