GLOBAL GEOMORPHOLOGY

Part I ☞ Introduction 
1. Approaches to geomorphology

Part II ☞ Endogenic processes and landforms 
2. Global morphology and tectonics 
3. Landforms and tectonics of plate margins 
4. Landforms and tectonics of plate interiors 
5. Landforms associated with igneous activity 

Part III ☞ Exogenic processes and landforms 
6. Weathering and associated landforms 
7. Slope processes and forms 
8. Fluvial processes 
9. Fluvial landforms 
10. Aeolian processes and landforms 
11. Glacial processes and landforms 
12. Periglacial processes and landforms 
13. Coastal processes and landforms 
14. Climate, climatic change and landform development 

Part IV ☞ Endogenic-exogenic interactions 
15. Rates of uplift and denudation 
16. Tectonics and drainage development 
17. Sea-level change 
18. Long-term landscape development 

Part V ☞ Extraterrestrial landforms 
19. Planetary geomorphology 

✸✸ OVERVIEW ✸✸

➤ This innovative text provides a comprehensive introduction to the subject of global geomorphology, with the emphasis placed on large-scale processes and phenomena. Integrating global tectonics into the study of landforms and incorporating planetary geomorphology as a major component the author discusses the impact of climatic change and the role of catastrophic events on landform genesis and includes a comprehensive study of surface geomorphic processes. 
DOWNLOAD
http://www.mediafire.com/file/yzia8a6ia6vaghs/Global_Geomorphology_%5BMichael_A._Summerfield%2C_2013%5D_%

FUDAMENTALS of INVERTEBRATE PALEONTOLOGY (MACROFOSSILS)

DOWNLOAD
http://www.mediafire.com/file/lwsqmkn39sxa86g/Fundamentals_of_Invertebrate_Palaeontology%2C_macrofossils_%5BSreepat_Jain%2C_2017%5D_%40

INTRODUCING MINERALOGY

1☞ The basics of mineralogy; 
2☞ Typical mineral occurrences; 
3☞ Atypical concentrations of minerals; 
4☞ Mineral collecting: where science and leisure overlap; 
5☞ Studying mineral assemblages and parageneses; 
6☞ Uses of minerals; 
7☞ Minerals and the environment. Epilogue. Glossary. Further reading and resources.

✸✸ OVERVIEW ✸✸
➤ this book introduces the essence of mineralogy. It begins with the basic chemistry of minerals and the way in which the mineral kingdom is classified. It then considers mineral occurrences, both typical, such as the minerals that largely make up common rocks like granite, and atypical, such as concentrations of rare metals in ore-deposits. The ways in which minerals are studied - using microscopes and the importance of careful observation and interpretation - are discussed, and the topics of mineral collecting and related issues are addressed. The final chapters of the book explore the uses of minerals, both industrial and scientific, and take a look at environmental issues associated with mineral extraction and usage. 
DOWNLOAD
http://www.mediafire.com/file/hj02np4xcd55o82/Introducing_Mineralogy_%5BJ

IRON ORE

1: Introduction☞ overview of the global iron ore industry
Part One☞ Characterization and analysis of iron ore
2☞ Mineralogical, chemical, and physical characteristics of iron ore
3☞ XRD analysis and evaluation of iron ores and sinters
4☞ Automated optical image analysis of natural and sintered iron ore
5☞ Quantitative analysis of iron ore using SEM-based technologies
6☞ Characterization of iron ore by visible and infrared reflectance and, Raman spectroscopies
7☞ Iron ore extraction techniques
8☞ Developments in iron ore comminution and classification technologies
9☞ Developments in the physical separation of iron ore: magnetic separation
10☞ Developments in nonmagnetic physical separation technologies for hematitic/goethitic iron ore
11☞ Developments in the physiochemical separation of iron ore
12☞ Developments in chemical separation of iron ore
13☞ Application of biotechnology in iron ore beneficiation
Part Three: Iron ore agglomeration processes and blast furnace iron-making technology
14☞ Iron ore sintering
15☞ Iron ore pelletization
16☞ Quality requirements of iron ore for iron production
17☞ Recent developments in blast furnace iron-making technology
Part Four☞ Environmental issues and low emission technologies
18☞ Sintering emissions and their mitigation technologies
19☞ Utilization of biomass as an alternative fuel in ironmaking
20☞ Life cycle assessment of iron ore mining and processing

DOWNLOAD
http://www.mediafire.com/file/dm5a6w0ab9s4ka3/Iron_Ore%2C_mineralogy%2C_processing_and_environmental_sustainability_%5BLiming

ISOTOPE GEOCHEMISTRY

Chapter 1: Atoms and nuclei: their physics and origins
Chapter 2: Decay systems and geochronology I
Chapter 3: Decay systems and geochronology II: U and Th
Chapter 4: Geochronology III: other dating methods
Chapter 5: Isotope cosmochemistry
Chapter 6: Radiogenic isotope geochemistry of the mantle
Chapter 7: Radiogenic isotope geochemistry of the continental crust and the oceans
Chapter 8: Stable isotope geochemistry I: Theory
Chapter 9: Stable isotope geochemistry II: High temperature applications
Chapter 10: Stable isotope geochemistry III: Low temperature applications
Chapter 11: Unconventional isotopes and approaches
Chapter 12: Noble gas isotope geochemistry

✸✸ OVERVIEW ✸✸

➤ This book provides a comprehensive introduction to radiogenic and stable isotope geochemistry.

DOWNLOAD

http://www.mediafire.com/…/Isotope_Geochemistry_%5BWilliam_…

GLOBOROTALIA ARCHEOMENARDII BOLLI 1957

Globorotalia archeomenardii BOLLI  1957

Referensi: Postuma Cenozoic halaman 316

Umur: N8-9 (Tentative correlation with European time-scale)

Zona Markers: -

Lokasi: Daerah Parengan LP 1

Batuan: Kalkarenit Lidah

Perbesaran mikroskop: 30 X

Deskripsi:

Test low trochospiral (terputar tidak pada satu bidang datar), biconvex (dwicembung), pipih, equatorial periphery (posisi apertur simetri, tepat diatas tepi periphery dari putaran awal cangkang planispiral) agak lobulated; periphery berada disekitar atau sepanjang sumbu lancip dengan/ tidak serupa dengan pseudo-keel.

Dinding test penuh dengan lubang-lubang yang kecil dengan permukaan yang halus.

Kamar-kamar test sangat pipih, tersusun dalam 3 putran; 4-5 kamar putaran terakhir bertambah dengan cepat dalam ukuran.

Sutur melengkung kuat, ramping tertekan sama rata/tinggi; umbilical (Posisi apertur pada awal test) pada sisi radial agak melengkung, tertekan.

Umbilicus  (Ruang yang dibentuk oleh tepi bagian dalam dinding umbilical dari kamar-kamar dalam suatu putaran yang sama) kecil, agak dangkal.

Apertur interiomarginal (Posisi apertur bukaan pada bagian dasar cangkang pada tepi kamar akhir, sepanjang sutur akhir), extraumbilical (Posisi apertur pada kamar akhir disepanjang sutura antara umbilicus dan periphery) dengan  low slit (Bentuk pipih memanjang)

Catatan tambahan: Globorotalia archeomenardii dapat dibedahkan dari Gt. menardii dan Gt. praemenardii yaitu lebih banyak cembung pada sisi spiral, kurang lobulated dan kecil

GEOLOGI DAERAH PARENGAN DAN SEKITARNYA KECAMATAN PARENGAN, KABUPATEN TUBAN PROPINSI JAWA TIMUR No Lembar Peta 4/9 1508 – 543 (Parengan)

INTISARI

Tujuan penelitian adalah untuk mengetahui keadaan geologi daerah penelitian, yang meliputi geomorfik, stratigrafi, geologi struktur, sejarah geologi, dan geologi lingkungan di daerah Parengan dan sekitarnya, Kecamatan Parengan, Kabupaten Tuban, Provinsi Jawa Timur yang  terletak pada koordinat 7^o02’30’’ LS – 7^o07’30’’ LS dan 111^o47’30” BT – 110^o52’30” BT.

Metode yang digunakan adalah dengan pemetaan geologi permukaan yang meliputi beberapa tahapan, antara lain tahap pendahuluan, tahap penelitian lapangan, tahap penelitian laboratorium, dan tahap akhir.

            Geomorfik daerah penelitian dibagi menjadi 4 subsatuan geomorfik, yaitu: subsatuan geomorfik dataran alluvial (F1), subsatuan geomorfik tubuh sungai (F2), perbukitan denudasional terkikis kuat (D1) dan subsatuan geomorfik perbukitan struktural terkikis sedang (S2). Pola pengaliran berupa dendritik dengan pola modifikasi subdendritik dan anastomotik, dengan stadia daerah dewasa-tua. Stratigrafi daerah penelitian terdiri dari 4 satuan dari yang paling tua sampai paling muda adalah, satuan batupasir karbonatan Ledok, satuan kalkarenit Mundu, satuan napal Mundu, satuan kalkarenit Lidah dan endapan campuran. Struktur geologi berupa sesar, kekar, dan lipatan . Sesar naik, yaitu Sesar Naik Parengan dan Sesar Naik Pacing, berarah relatif timurlaut-baratdaya. Sesar Mendatar Kiri Parengan yang berarah relatif timurlaut-baratdaya. Potensi geologi daerah penelitian berupa air, dan bahan galian pasir dan batu (sirtu), kalkarenit dan napal. Bencana alam berupa banjir, gerakan massa, kekeringan dan angin puting beliung. Potensi energi terbarukan berupa energi biogas, PLTA dan PLTS, juga terdapat situs arkeologi berupa sarkofagus.

Kata Kunci: Kecamatan Parengan, geologi Parengan, potensi geologi

                    Parengan, bencana alam.

 ABSTRACT

The research objective was to determine the state of regional geological studies, which include geomorphology, stratigraphy, structural geology, historical geology and environmental geology, located in Parengan and surrounding area, district Parengan, Tuban, East Java Province. The astronomical located at coordinates 7^o02'30'' SL-7^o07'30''SL and 111^o47'30 "EL- 110^o52'30"EL.

            The method used is with surface geologic mapping which includes several stages, including a pre-field stage, the stage surface geological mapping, laboratory analysis phase, studio analysis phase, the data synthesis stage and the stage of preparation of final report.

            Geomorphology in the study area is divided into 4 subunits geomorphology, namely: subunits river geomorphology body (F2), alluvial plains geomorphology sub unit (F1), the hills denudasional (D1) and geomorphology of the complex folds of denudation (S2).  Dendritic drainage pattern in the form of a pattern modification subdendritik and anastomotik, the stadia-old adult area. Stratigraphy study area consists of 4 lithologies are Ledok calcareous sandstone unit, Mundu kalkarenit unit, Mundu marl unit, Lidah kalkarenit unit, and sediment mixture. Geological structures developed in research areas such as faults, joints, and folds. Fault is Reverse Fault Parengan and Reverse Fault Pacing, relative trending northeast-southwest. Left Horizontal  Fault relative Parengan trending northeast-northwest. Geological potential of research areas such as water, sand and stone minerals (gravel), kalkarenit and marl. Natural disasters such as floods, droughts and whirling wind. The potential of renewable energy such as biogas, hydropower and solar power, there are also archaeological sites in the form of a sarcophagus.

Keywords:   District of Parengan, geology Parengan,  potential geological

                    Parengan, natural disasters.