Nama Lengkap : Dr. Ir. Mohamad Sapari Dwi Hadian, ST., MT

E-mail : [email protected]

Bidang Keahlian : Geologi Lingkungan

Prodi S3 Calon Mahasiswa: Doktor Geologi 

Judul Penelitian yang Ditawarkan:

RESPON KONTROL DEPOSIT ALLUVIAL MELALUI PENDEKATAN SINTETIK DAN IMPLEMENTASINYA TERHADAP SUBSURFACE FLOW

ALLUVIAL DEPOSIT CONTROL RESPONSE THROUGH A SYNTHETIC APPROACH AND ITS IMPLEMENTATION TO SUBSURFACE FLOW

 

Abstrak:

Dinamika internal sedimentasi aluvial pada cekungan berperan dalam mengontrol proses sedimentasi pada suatu ekosistem lingkungan, tidak terlepas juga pada lingkungan sedimentasi alluvial dalam proporsi ruang dan waktu yang berbeda menjadikan interaksi kedua dinamika ini pada stratigrafi alluvial menjadi kompleks hal ini dikontrol oleh allogenic berskala global, sedangkan kontrol autogenic seringkali bersifat chaos dan local. Dengan memahami respon kontrol autogenic pada rekaman stratigrafi, maka tidak hanya korelasi regional namun juga variasi atau dinamika lokal sedimentasi dapat terpetakan secara komprehensif. Pendekomposisian kedua kontrol ini dari data stratigrafi masih merupakan suatu tantangan. Di samping itu, baik kontrol autogenic maupun allogenic keduanya dapat membentuk siklisitas yang serupa. Pemodelan fisis maupun eksperimen telah banyak isimulasikan untuk mengetahui interaksi dinamika autogenic dan allogenic. Tetapi, pendekatan semacam ini menyisakan keterbatasan ketika diimplementasikan pada data riil. Sejumlah parameter di alam yang tidak diketahui menjadi limitasi. Oleh karenanya, beberapa pertanyaan muncul yang menjadi konsentrasi dalam penelitian ini. adapun penelitian ini untuk menjawab problematika Karakter siklisitas stratigrafi alluvial akibat kontrol internal dan eksternal, Model merekonstruksi siklisitas stratigrafi alluvial, dan implementasi dan reinterpretasi melalui algoritma data.

Abstract:

The internal dynamics of alluvial sedimentation in the basin plays a role in controlling the sedimentation process in an environmental ecosystem, it is also inseparable from the alluvial sedimentation environment in different proportions of space and time making the interaction of these two dynamics in stratigraphy. The internal dynamics of alluvial sedimentation in the basin plays a role in controlling the sedimentation process in an environmental ecosystem, it is also inseparable from the alluvial sedimentation environment in different proportions of space and time making the interaction of these two dynamics in stratigraphy. alluvial becomes complex, this is controlled by allogenic on a global scale, while autogenic control is often chaotic and local. By understanding the response of autogenic controls on stratigraphic records, not only regional correlations but also variations or local dynamics of sedimentation can be mapped comprehensively. the decomposition of these two controls from the stratigraphic data is still a challenge. In addition, both autogenic and allogenic controls can form a similar cyclicity. Many physical and experimental models have been simulated to determine the interaction of autogenic and allogenic dynamics. However, this kind of approach leaves limitations when implemented in real data. A number of parameters in nature that are not known to be a limitation. Therefore, several questions arise that become the focus of this research. As for this study to answer the problem of alluvial stratigraphic cyclicity character due to internal and external controls, the model reconstructs alluvial stratigraphic cyclicity, and implementation and reinterpretation through data algorithms. alluvial becomes complex, this is controlled by allogenic on a global scale, while autogenic control is often chaotic and local. By understanding the response of autogenic controls on stratigraphic records, not only regional correlations but also variations or local dynamics of sedimentation can be mapped comprehensively. the decomposition of these two controls from the stratigraphic data is still a challenge. In addition, both autogenic and allogenic controls can form a similar cyclicity. Many physical and experimental models have been simulated to determine the interaction of autogenic and allogenic dynamics. However, this kind of approach leaves limitations when implemented in real data. A number of parameters in nature that are not known to be a limitation. Therefore, several questions arise that become the focus of this research. As for this study to answer the problem of alluvial stratigraphic cyclicity character due to internal and external controls, the model reconstructs alluvial stratigraphic cyclicity, and implementation and reinterpretation through data algorithms.